Seismic structure and tectonics of the Alasehir--Gediz Graben, Western Turkey

Science.gov (United States)

Turk, Sezer

The Aegean Extensional Province (AEP) in Western Anatolia includes three major graben systems that have formed as a result of N-S tectonic extension in the latest Cenozoic. The 6 to 30-km-wide Alasehir--Gediz Graben (AGG) in the north contains ˜3-km-thick Miocene and Plio-Quaternary, alluvial--fluvial and lacustrine sedimentary rocks. I have used seismic profiles, well-log data and the regional stratigraphy to identify the key stratigraphic units, their bounding surfaces and vertical thicknesses, and to document the subsurface structural architecture of the AGG. A north-dipping detachment fault exposed in the southern shoulder of the AGG basin occurs at 2--2.5 km at depth beneath the graben fill, and is dissected by ˜E--W--striking, synthetic to antithetic, high-angle normal faults. The graben system is crosscut by NNE-oriented cross faults, showing several km of recurrence interval and 10s of meters of vertical displacement. These faults divide the graben into several sub-basins and display positive and negative flower structures. The structural architecture in the sub-basins shows important variations in stratigraphic thicknesses, fault geometry-displacement and deformation patterns, indicating that cross faulting played a critical role in the evolution of the AAG.

Morphostructural evidence for Recent/active extension in Central Tanzania beyond the southern termination of the Kenya Rift.

Science.gov (United States)

Le Gall, B.; Rolet, J.; Gernigon, L.; Ebinger, C.; Gloaguen, R.

2003-04-01

The southern tip zone of the Kenya Rift on the eastern branch of the East African System is usually thought to occur in the so-called North Tanzanian Divergence. In this region, the narrow (50 km-wide) axial graben of southern Kenya splays southwards, via a major EW-trending volcanic lineament, into a 200 km-wide broad rifted zone with three separate arms of normal faulting and tilted fault blocks (Eyasi, Manyara and Pangani arms from W to E). Remote sensing analysis from Central Tanzania demonstrates that rift morphology exists over an area lying 400 km beyond the southern termination of the Kenya Rift. The most prominent rift structures are observed in the Kilombero region and consist of a 100 km-wide range of uplifted basement blocks fringed to the west by an E-facing half-graben inferred to reach depths of 6-8 km from aeromagnetic dataset. Physiographic features (fault scarps), and river drainage anomalies suggest that the present-day rift pattern in the Kilombero extensional province principally results from Recent/Neogene deformation. That assumption is also supported by the seismogenic character of a number of faults. The Kilombero half-graben is superimposed upon an earlier rift system, Karoo in age, which is totally overprinted and is only evidenced from its sedimentary infill. On the other hand, the nature and thickness of the inferred Neogene synrift section is still unknown. The Kilombero rifted zone is assumed to connect northwards into the central rift arm (Manyara) of the South Kenya Rift via a seismically active transverse fault zone that follows ductile fabrics within the Mozambican crystalline basement. The proposed rift model implies that incipient rifting propagates hroughout the cold and strong crust/lithosphere of Central Tanzania along Proterozoic (N140=B0E) basement weakness zones and earlier Karoo (NS)rift structures. A second belt of Recent-active linked fault/basins also extends further East from the Pangani rift arm to the offshore

The relation of catastrophic flooding of Mangala Valles, Mars, to faulting of Memnonia Fossae and Tharsis volcanism

International Nuclear Information System (INIS)

Tanaka, K.L.; Chapman, M.G.

1990-01-01

Detailed stratigraphic relations indicate two coeval periods of catastrophic flooding and Tharsis-centered faulting (producing Memnonia Fossae) in the Mangala Valles region of Mars. Major sequences of lava flows of the Tharsis Montes Formation and local, lobate plains flows were erupted during and between these channeling and faulting episodes. First, Late Hesperian channel development overlapped in time the Tharsis-centered faulting that trends north 75 degree to 90 degree E. Next, Late Hesperian/Early Amazonian flooding was coeval with faulting that trends north 55 degree to 70 degree E. In some reaches, resistant lava flows filled the early channels, resulting in inverted channel topography after the later flooding swept through. Both floods likely originated from the same graben, which probably was activated during each episode of faulting. Faulting broke through groundwater barriers and tapped confined aquifers in higher regions west and east of the point of discharge. The minimum volume of water required to erode Mangala Valles (about 5 x 10 12 m 3 ) may have been released through two floods that drained a few percent pore volume from a relatively permeable aquifer. The peak discharges of the floods may have lasted from days to weeks. The perched water discharged from the aquifer may have been produced by hydrothermal groundwater circulation induced by Tharsis magmatism, tectonic uplift centered at Tharsis Montes, and compacting of saturated crater ejecta due to loading by lava flows

Acoustic stratigraphy of Bear Lake, Utah-Idaho: late Quaternary sedimentation patterns in a simple half-graben

Science.gov (United States)

Colman, Steven M.

2006-01-01

A 277-km network of high-resolution seismic-reflection profiles, supplemented with a sidescan-sonar mosaic of the lake floor, was collected in Bear Lake, Utah–Idaho, in order to explore the sedimentary framework of the lake's paleoclimate record. The acoustic stratigraphy is tied to a 120 m deep, continuously cored drill hole in the lake. Based on the age model for the drill core, the oldest continuously mapped acoustic reflector in the data set has an age of about 100 ka, although older sediments were locally imaged. The acoustic stratigraphy of the sediments below the lake indicates that the basin developed primarily as a simple half-graben, with a steep normal-fault margin on the east and a flexural margin on the west. As expected for a basin controlled by a listric master fault, seismic reflections steepen and diverge toward the fault, bounding eastward-thickening sediment wedges. Secondary normal faults west of the master fault were imaged beneath the lake and many of these faults show progressively increasing offset with depth and age. Several faults cut the youngest sediments in the lake as well as the modern lake floor. The relative simplicity of the sedimentary sequence is interrupted in the northwestern part of the basin by a unit that is interpreted as a large (4 × 10 km) paleodelta of the Bear River. The delta overlies a horizon with an age of about 97 ka, outcrops at the lake floor and is onlapped by much of the uppermost sequence of lake sediments. A feature interpreted as a wave-cut bench occurs in many places on the western side of the lake. The base of this bench occurs at a depth (22–24 m) similar to that (20–25 m) of the distal surface of the paleodelta. Pinch-outs of sedimentary units are common in relatively shallow water on the gentle western margin of the basin and little Holocene sediment has accumulated in water depths of less than 30 m. On the steep eastern margin of the basin, sediments commonly onlap the hanging wall of the East

The Jurassic of Denmark and Greenland: Sedimentology and sequence stratigraphy of paralic and shallow marine Upper Jurassic sandstones in the northern Danish Central Graben

Directory of Open Access Journals (Sweden)

Johannessen, Peter N.

2003-10-01

Full Text Available Paralic and shallow marine sandstones were deposited in the Danish Central Graben during Late Jurassic rifting when half-grabens were developed and the overall eustatic sea level rose. During the Kimmeridgian, an extensive plateau area consisting of the Heno Plateau and the Gertrud Plateau was situated between two highs, the Mandal High to the north, and the combined Inge and Mads Highs to the west. These highs were land areas situated on either side of the plateaus and supplied sand to the Gertrud and Heno Plateaus. Two graben areas, the Feda and Tail End Grabens, flanked the plateau area to the west and east, respectively. The regressive–ransgressive succession consists of intensely bioturbated shoreface sandstones, 25–75 m thick. Two widespread unconformities (SB1, SB2 are recognised on the plateaus, forming the base of sequence 1 and sequence 2, respectively. These unconformities were created by a fall in relative sea level during which rivers may have eroded older shoreface sands and transported sediment across the Heno andGertrud Plateaus, resulting in the accumulation of shoreface sandstones farther out in the Feda and Tail End Grabens, on the south-east Heno Plateau and in the Salt Dome Province. Duringsubsequent transgression, fluvial sediments were reworked by high-energy shoreface processes on the Heno and Gertrud Plateaus, leaving only a lag of granules and pebbles on the marine transgressive surfaces of erosion (MTSE1, MTSE2.The sequence boundary SB1 can be traced to the south-east Heno Plateau and the Salt Dome Province, where it is marked by sharp-based shoreface sandstones. During low sea level, erosion occurred in the southern part of the Feda Graben, which formed part of the Gertrud and Heno Plateaus, and sedimentation occurred in the Norwegian part of the Feda Graben farther to the north. During subsequent transgression, the southern part of the Feda Graben began to subside, and a succession of backstepping back

Downthrown traps of the NW Witch Ground Graben, UK North Sea

Energy Technology Data Exchange (ETDEWEB)

Hindle, A.D. (Texaco Ltd., London (GB))

1989-10-01

The structures drilled to-date in the NW Witch Ground Graben area have been assigned to two broad categories: upthrown traps with four-way dip closure or tilted fault blocks, generally located on the flanks of the graben; and downthrown traps with closure against a major fault, located downthrown on the main graben border-fault systems. Many of these are in fact combination traps, having upthrown fault-seal and/or stratigraphic elements. A study of trap settings has shown: the success rate for encountering hydrocarbons in upthrown traps and downthrown traps is very similar; the common belief that the footwall seal is the most critical element of a downthrown trap is questionable; modern seismic data reveals that a high proportion of unsuccessful exploratory wells were not located on a closed structure; there is a lesser chance of the reservoir being absent, or there being no migration route to the trap, in downthrown compared with upthrown structures; carboniferous sediments can be a footwall seal for a downthrown trap in one location, and a reservoir for hydrocarbons in another; the structural evolution of the Graben has been ideal for the development of downthrown traps. (author).

Graben calderas of the Sierra Madre Occidental: The case of Guanajuato, central Mexico

Science.gov (United States)

Aguirre-Diaz, G. J.; Tristán-González, M.; Labarthe-Hernández, G.; Marti, J.

2013-12-01

The Sierra Madre Occidental (SMO) volcanic province is characterized by voluminous silicic ignimbrites that reach an accumulated thickness of 500 to 1500 m. A single ignimbrite can reach up to 350 m thick in its outflow facies. This ignimbrite sequence formed mostly within 38-23 Ma, building up a total estimated volume of ca. 580,000 km3 making the SMO the largest ignimbrite province of the world. We have showed that several and probably most of the SMO ignimbrites were erupted from fissures associated to Basin and Range fault systems or grabens (Geology, 2003), thus naming these volcano-tectonic structures as graben calderas (Caldera Volcanism book, Elsevier, 2008). Generally, the sequence observed in graben calderas include, from oldest to youngest, alluvial fan deposits combined with lacustrine deposits, pyroclastic surge deposits and minor volume ignimbrites, a large-volume ignimbrite that could be massive or made of successive layers, and sometimes silicic lava domes and/or mafic fissural lavas both with vents aligned with the graben trend. Fallout deposits, plinian or non-plinian, are not observed in the sequence. Thus, onset of caldera collapse represented by the major ignimbrite must occur just after deposition of continental sediments within the graben domain. A similar volcano-tectonic development is observed in pull-apart grabens. Therefore, extensional or transtensional tectonics, before and during caldera collapse, and the emplacement of a subgraben shallow silicic magma chamber are the necessary conditions for the development of graben calderas. We describe here the case of the Guanajuato graben caldera, located in the central part of Mexico and in the southeastern portion of the SMO volcanic province. The caldera is part of the economically important mining district of Guanajuato, with 28 silver mines, some active since the 16th century. The caldera structure, a rectangle of 10 x 16 km, was controlled by NW and NE regional fault systems. Most ore

The geothermal conditions in the Rhine Graben - a summary

Energy Technology Data Exchange (ETDEWEB)

Rybach, L.

2007-07-15

This article takes a look at the situation in the upper Rhine valley with respect to its geothermal potential. The Rhine Graben, being part of the European Mid-Continental Rift System is characterised by thinned crust and therefore higher heat flow rates. According to the author, the Rhine Graben presents generally favourable conditions for geothermal energy development and utilisation. This illustrated article presents information on the geological structures to be found and figures obtained from the geothermal exploration project at Soulz-sous-Forets, France, and a number of other geothermal investigation and production projects in Germany.

Geothermal Exploration of the Winston Graben, Central New Mexico, USA

Science.gov (United States)

Sophy, M. J.; Kelley, S. A.

2011-12-01

We are assessing the geothermal potential of the Winston Graben of central New Mexico using borehole temperature logs and geophysical data. The Winston Graben is a late Cenozoic rift basin, part of the larger Rio Grande rift, which is 5 to 10 km wide and 56 km long with northern and southern termini occurring at accommodation zones that coincide with late Cenozoic volcanic lineaments. The graben is interpreted to be symmetric based on geologic mapping, with 2 km of stratigraphic offset on both the western and eastern margins. The graben is bordered by the Black Range to the west and is separated from the Rio Grande valley by the Sierra Cuchillo, a horst block made of Paleozoic rocks intruded by a laccolith. Geothermal and geophysical data, including water table measurements, well temperature logs, thermal conductivity samples, bottom hole temperatures, water chemistry, and gravity data have been extracted from the New Mexico Geothermal Database, part of the National Geothermal Database, and the Geonet Gravity and Magnetic Dataset Repository. Combined with existing geologic maps of the Winston Graben and surroundings, these data help to identify spatial relationships between geologic structures and groundwater parameters and distribution. Geothermal gradients from industry temperature-depth well profiles range from 20°C/km to 60°C/km with a spatial distribution of higher gradients located on the eastern side of the Sierra Cuchillo horst, which is where a mapped warm spring is located. Lower thermal gradients were observed to the west in the groundwater recharge area of the basin. Analysis of Bouguer gravity data indicate a gravity low coinciding with the center of the Winston Graben, which is attributed to be the deepest part of the basin, symetrically surrounded by gravity highs. Gravity highs coincide with the middle Cenozoic Morenci and Chise volcanic lineaments along the northern and southern ends of the graben. The mapped warm spring occurs at the

A Middle-Upper Miocene fluvial-lacustrine rift sequence in the Song Ba Rift, Vietnam

DEFF Research Database (Denmark)

Lars H., Nielsen; Henrik I., Petersen; Nguyen D., Dau

2007-01-01

The small Neogene Krong Pa graben is situated within the continental Song Ba Rift, which is bounded by strike-slip faults that were reactivated as extensional faults in Middle Miocene time. The 500 m thick graben-fill shows an overall depositional development reflecting the structural evolution...... subsidence rate and possibly a higher influx of water from the axial river systems the general water level in the graben rose and deep lakes formed. High organic preservation in the lakes prompted the formation of two excellent oil-prone lacustrine source-rock units. In the late phase of the graben...... as carrier beds, whereas the braided fluvial sandstones and conglomerates along the graben margins may form reservoirs. The Krong Pa graben thus contains oil-prone lacustrine source rocks, effective conduits for generated hydrocarbons and reservoir sandstones side-sealed by the graben faults toward...

The deep thermal field of the Upper Rhine Graben

Science.gov (United States)

Freymark, Jessica; Sippel, Judith; Scheck-Wenderoth, Magdalena; Bär, Kristian; Stiller, Manfred; Fritsche, Johann-Gerhard; Kracht, Matthias

2017-01-01

The Upper Rhine Graben has a significant socioeconomic relevance as it provides a great potential for geothermal energy production. The key for the utilisation of this energy resource is to understand the controlling factors of the thermal field in this area. We have therefore built a data-based lithospheric-scale 3D structural model of the Upper Rhine Graben and its adjacent areas. In addition, 3D gravity modelling was performed to constrain the internal structure of the crystalline crust consistent with seismic information. Based on this lithosphere scale 3D structural model the present-day conductive thermal field was calculated and compared to measured temperatures. Our results show that the regional thermal field is mainly controlled by the configuration of the upper crust, which has different thermal properties characteristic for the Variscan and Alpine domains. Temperature maxima are predicted for the Upper Rhine Graben where thick insulating Cenozoic sediments cause a thermal blanketing effect and where the underlying crustal units are characterised by high radiogenic heat production. The comparison of calculated and measured temperatures overall shows a reasonable fit, while locally occuring model deviations indicate where a larger influence of groundwater flow may be expected.

Graben formation during the Bárðarbunga rifting event in central Iceland

KAUST Repository

Ruch, Joel; Jonsson, Sigurjon; Wang, Teng; Xu, Wenbin; Trippanera, Daniele

2015-01-01

to the dike emplacement in the shallow crust, which generated in few days an 8 km long by 0.8 km wide graben (depression) structure. The new graben extends from the northern edge of the Vatnajökull glacier and to the north to the eruptive fissure. We analyze

Fault and graben growth along active magmatic divergent plate boundaries in Iceland and Ethiopia

KAUST Repository

Trippanera, D.; Acocella, V.; Ruch, Joel; Abebe, B.

2015-01-01

Recent studies highlight the importance of annual-scale dike-induced rifting episodes in developing normal faults and graben along the active axis of magmatic divergent plate boundaries (MDPB). However, the longer-term (102-105 years) role of diking on the cumulative surface deformation and evolution of MDPB is not yet well understood. To better understand the longer-term normal faults and graben along the axis of MDPB, we analyze fissure swarms in Iceland and Ethiopia. We first focus on the simplest case of immature fissure swarms, with single dike-fed eruptive fissures; these consist of a <1 km wide graben bordered by normal faults with displacement up to a few meters, consistent with theoretical models and geodetic data. A similar structural pattern is found, with asymmetric and multiple graben, within wider mature fissure swarms, formed by several dike-fed eruptive fissures. We then consider the lateral termination of normal faults along these graben, to detect their upward or downward propagation. Most faults terminate as open fractures on flat surface, suggesting downward fault propagation; this is consistent with recent experiments showing dike-induced normal faults propagating downward from the surface. However, some normal faults also terminate as open fractures on monoclines, which resemble fault propagation folds; this suggests upward propagation of reactivated buried faults, promoted by diking. These results suggest that fault growth and graben development, as well as the longer-term evolution of the axis of MDPB, may be explained only through dike emplacement and that any amagmatic faulting is not necessary.

Fault and graben growth along active magmatic divergent plate boundaries in Iceland and Ethiopia

KAUST Repository

Trippanera, D.

2015-10-08

Recent studies highlight the importance of annual-scale dike-induced rifting episodes in developing normal faults and graben along the active axis of magmatic divergent plate boundaries (MDPB). However, the longer-term (102-105 years) role of diking on the cumulative surface deformation and evolution of MDPB is not yet well understood. To better understand the longer-term normal faults and graben along the axis of MDPB, we analyze fissure swarms in Iceland and Ethiopia. We first focus on the simplest case of immature fissure swarms, with single dike-fed eruptive fissures; these consist of a <1 km wide graben bordered by normal faults with displacement up to a few meters, consistent with theoretical models and geodetic data. A similar structural pattern is found, with asymmetric and multiple graben, within wider mature fissure swarms, formed by several dike-fed eruptive fissures. We then consider the lateral termination of normal faults along these graben, to detect their upward or downward propagation. Most faults terminate as open fractures on flat surface, suggesting downward fault propagation; this is consistent with recent experiments showing dike-induced normal faults propagating downward from the surface. However, some normal faults also terminate as open fractures on monoclines, which resemble fault propagation folds; this suggests upward propagation of reactivated buried faults, promoted by diking. These results suggest that fault growth and graben development, as well as the longer-term evolution of the axis of MDPB, may be explained only through dike emplacement and that any amagmatic faulting is not necessary.

Upper bounds of deformation in the Upper Rhine Graben from GPS data - First results from GURN (GNSS Upper Rhine Graben Network)

Science.gov (United States)

Masson, Frederic; Knoepfler, Andreas; Mayer, Michael; Ulrich, Patrice; Heck, Bernhard

2010-05-01

In September 2008, the Institut de Physique du Globe de Strasbourg (Ecole et Observatoire des Sciences de la Terre, EOST) and the Geodetic Institute (GIK) of Karlsruhe University (TH) established a transnational cooperation called GURN (GNSS Upper Rhine Graben Network). Within the GURN initiative these institutions are cooperating in order to establish a highly precise and highly sensitive network of permanently operating GNSS sites for the detection of crustal movements in the Upper Rhine Graben region. At the beginning, the network consisted of the permanently operating GNSS sites of SAPOS®-Baden-Württemberg, different data providers in France (e.g. EOST, Teria, RGP) and some further sites (e.g. IGS). In July 2009, the network was extended to the South when swisstopo (Switzerland) and to the North when SAPOS®-Rheinland-Pfalz joined GURN. Therefore, actually the GNSS network consists of approx. 80 permanently operating reference sites. The presentation will discuss the actual status of GURN, main research goals, and will present first results concerning the data quality as well as time series of a first reprocessing of all available data since 2002 using GAMIT/GLOBK (EOST working group) and the Bernese GPS Software (GIK working group). Based on these time series, the velocity as well as strain fields will be calculated in the future. The GURN initiative is also aiming for the estimation of the upper bounds of deformation in the Upper Rhine Graben region.

Anfibios y reptiles del valle del Mezquital, Hidalgo, México Amphibians and reptiles from the Valle del Mezquital, Hidalgo, Mexico

Directory of Open Access Journals (Sweden)

Leonardo Fernández-Badillo

2010-12-01

Full Text Available El valle del Mezquital, Hidalgo, México, es un área de gran riqueza biológica; sin embargo, se desconoce mucho sobre su herpetofauna, por lo que se realizó una lista de anfibios y reptiles de 3 zonas del valle. Se analizó su distribución por tipo de vegetación, se registraron los microhábitats utilizados, así como la abundancia relativa. Se llevaron a cabo 12 salidas mensuales durante 1 año, con 108 días de muestreo. Se realizaron recorridos sobre transectos, en 9 tipos de vegetación. La herpetofauna del área de estudio está integrada por 37 especies (7 anfibios y 30 reptiles, de las cuales 8 se registran por primera vez para el valle del Mezquital. La mayoría de las especies se presentaron en las zonas de cultivo (26, 14 especies en los de la zona templada y 13 en los de la zona de riego. La herpetofauna del valle del Mezquital utiliza un total de 27 tipos de microhábitats, siendo "bajo roca" donde se registró el mayor número de especies (22. La mayoría de las especies tanto de anfibios como de reptiles fueron consideradas raras.Valle del Mezquital Hidalgo, Mexico is known for its high biological richness, but little is known about its herpetofauna. A study to list the amphibians and reptiles of 3 different zones at the Valle del Mezquital was carried out. We analyzed their distribution in different types of vegetation, their microhabitat and relative abundance in 12 monthly trips during 1 year for a total of 108 days. We sampled transects over 9 types of vegetation. Thirty species have been reported for this area (7 amphibians, 30 reptiles, 8 reported for the first time from Valle del Mezquital. Most of the species were present within crops (26, 14 within the temperate zone and 13 within the irrigation zone. The herpetofauna at Valle del Mezquital uses 27 different microhabitat, being "under rock" the most used by 22 species. Most of the species, both amphibians and reptiles were considered rare.

Boundary separating the seismically active reelfoot rift from the sparsely seismic Rough Creek graben, Kentucky and Illinois

Science.gov (United States)

Wheeler, R.L.

1997-01-01

The Reelfoot rift is the most active of six Iapetan rifts and grabens in central and eastern North America. In contrast, the Rough Creek graben is one of the least active, being seismically indistinguishable from the central craton of North America. Yet the rift and graben adjoin. Hazard assessment in the rift and graben would be aided by identification of a boundary between them. Changes in the strikes of single large faults, the location of a Cambrian transfer zone, and the geographic extent of alkaline igneous rocks provide three independent estimates of the location of a structural boundary between the rift and the graben. The boundary trends north-northwest through the northeastern part of the Fluorspar Area Fault Complex of Kentucky and Illinois, and has no obvious surface expression. The boundary involves the largest faults, which are the most likely to penetrate to hypocentral depths, and the boundary coincides with the geographic change from abundant seismicity in the rift to sparse seismicity in the graben. Because the structural boundary was defined by geologic variables that are expected to be causally associated with seismicity, it may continue to bound the Reelfoot rift seismicity in the future.

Stratigraphy of the Kasei Valles region, Mars

Science.gov (United States)

Robinson, Mark S.; Tanaka, Kenneth L.

1987-01-01

The thicknesses and geomorphology of the two principal stratigraphic units exposed in Kasei Valles to aid in interpreting the nature of crustal materials and the history of the channeling events in the area are identified and described. Previous studies of Kasei Valles have related the channel landforms to glacial flow, catastrophic flooding, and large-scale eolian erosion. The two units (an upper and a lower unit) form thick sheets, each having distinct geomorphologic features. Thicknesses of the unit were determined through preliminary stereogrammetric profiles taken across many sections of western Kasei Valles and shadow measurements taken of scarp heights from calibrated Viking images having sun angles less than 25 degrees; DN values were examined to confirm that true shadows were observed.

Marine intervals in Neogene fluvial deposits of western Amazonia

Science.gov (United States)

Boonstra, Melanie; Troelstra, Simon; Lammertsma, Emmy; Hoorn, Carina

2014-05-01

Amazonia is one of the most species rich areas on Earth, but this high diversity is not homogeneous over the entire region. Highest mammal and tree-alpha diversity is found in the fluvio-lacustrine Pebas system, a Neogene wetland associated with rapid radiation of species. The estuarine to marine origin of various modern Amazonian fish, plants, and invertebrates has been associated with past marine ingressions into this freshwater Pebas system. The exact nature and age of these invasions is, however, debated. Here we present new evidence from fluvial and fluvio-lacustrine deposits of Neogene age in southeast Colombia, that point to periods of widespread marine conditions in western Amazonia. Our evidence is based on an analysis of marine palynomorphs, such as organic linings of foraminifera and dinoflagellate cysts, present in dark sandy clay sediments that outcrop along the Caqueta and Amazon rivers. Characteristically, the foraminiferal linings can be assigned to three benthic morphotypes only, e.g. Ammonia, Elphidium and Trochammina. This low diversity assemblage is associated with estuarine/marginal marine conditions. No distinct marine elements such as shelf or planktonic species were encountered. The observed foraminiferal linings and dinocyst assemblages are typical for a (eutrophic) shallow marine environment, suggesting that the Pebas freshwater wetland system occasionally changed to (marginal) marine. Although some reworked elements are found, a typical Neogene dinocyst taxon is commonly found supporting in situ deposition. Sedimentological features typical for tidal conditions that are reported for sites in Peru and northeastern Brazil likely relate to these marine ingressions. Sea level changes as well as foreland basin development related to Andes formation may have facilitated the entry of marine water during the Neogene.

Neogene dinocyst zonation for the eastern North Sea Basin, Denmark

DEFF Research Database (Denmark)

Dybkjær, Karen; Piasecki, Stefan

2010-01-01

A dinocyst zonation for the Neogene succession in the eastern part of the North Sea Basin (Denmark) is presented. The zonation is based on an extensive database comprising data from more than fifty onshore and offshore boreholes and about twenty five outcrops. Most of the nineteen dinocyst zones......, of the Lower Miocene, and of the Upper Miocene and Pliocene successions. The previous zonation of the onshore Danish Middle Miocene is reconsidered and partly redefined. The zonation is correlated with other biostratigraphic subdivisions of the Neogene succession in the Danish region in addition to litho...

Modelling of hydrothermal fluid flow and structural architecture in an extensional basin, Ngakuru Graben, Taupo Rift, New Zealand

Science.gov (United States)

Kissling, W. M.; Villamor, P.; Ellis, S. M.; Rae, A.

2018-05-01

Present-day geothermal activity on the margins of the Ngakuru graben and evidence of fossil hydrothermal activity in the central graben suggest that a graben-wide system of permeable intersecting faults acts as the principal conduit for fluid flow to the surface. We have developed numerical models of fluid and heat flow in a regional-scale 2-D cross-section of the Ngakuru Graben. The models incorporate simplified representations of two 'end-member' fault architectures (one symmetric at depth, the other highly asymmetric) which are consistent with the surface locations and dips of the Ngakuru graben faults. The models are used to explore controls on buoyancy-driven convective fluid flow which could explain the differences between the past and present hydrothermal systems associated with these faults. The models show that the surface flows from the faults are strongly controlled by the fault permeability, the fault system architecture and the location of the heat source with respect to the faults in the graben. In particular, fault intersections at depth allow exchange of fluid between faults, and the location of the heat source on the footwall of normal faults can facilitate upflow along those faults. These controls give rise to two distinct fluid flow regimes in the fault network. The first, a regular flow regime, is characterised by a nearly unchanging pattern of fluid flow vectors within the fault network as the fault permeability evolves. In the second, complex flow regime, the surface flows depend strongly on fault permeability, and can fluctuate in an erratic manner. The direction of flow within faults can reverse in both regimes as fault permeability changes. Both flow regimes provide insights into the differences between the present-day and fossil geothermal systems in the Ngakuru graben. Hydrothermal upflow along the Paeroa fault seems to have occurred, possibly continuously, for tens of thousands of years, while upflow in other faults in the graben has

The Late Variscan control on the location and asymmetry of the Upper Rhine Graben

Science.gov (United States)

Grimmer, J. C.; Ritter, J. R. R.; Eisbacher, G. H.; Fielitz, W.

2017-04-01

The NNE-trending Upper Rhine Graben (URG) of the European Cenozoic Rift System developed from c. 47 Ma onwards in response to changing lithospheric stresses in the northwestern foreland of the Alps. The composite graben structure consists of three segments, each c. 100 km long and 30-40 km wide, but flares to c. 60 km near its southern and to c. 80 km near its northern termination. Normal faulting induced a total extension of 5-8 km of the 1-2 km thick Mesozoic sedimentary Franconian platform and underlying Variscan basement rocks. However, distribution of an up to 3.5 km thick sedimentary graben fill and cumulative displacements near Eastern and Western Main Border fault systems suggest that subsidence of the graben floor and shoulder uplift created strong cross-sectional asymmetries. Cumulative W-down displacements >3 km along strongly segmented transfer faults in the east contrast with E-down displacements emergence of the platform above sea level in late Mesozoic times, the deep-reaching W-dipping "extensional defects" of the East Rhine Detachment exerted a primary lithospheric scale control on both location and cross-sectional asymmetry of the Cenozoic graben structure. NE- and NW-striking, strongly altered and more shallow rooted Permocarboniferous or Mesozoic faults exerted secondary upper crustal controls on transfer faults and the accommodation zones near the terminations and segment boundaries of the URG. Deep crustal to upper lithospheric asymmetries continue to influence the neotectonic setting of the URG, such as westward rising earthquake hypocentres. Seismic activity along the URG appears to be part of a >600 km long zone that delimits the trailing edge of a SW-moving lithospheric block. In the URG area, NE-SW-oriented seismic anisotropy at sublithospheric depths of c. 60-80 km suggest active mantle flow in this direction as a possible driving force for the reactivation of pre-graben lithospheric shear zones.

Aeromagnetic Study of the Nortern Acambay Graben and Amealco Caldera, Central Mexican Volcanic Belt

Science.gov (United States)

Gonzalez, T.

2011-12-01

The Mexican Volcanic Belt (MVB) is characterized by E-W striking faults which form a series of en echelon graben along its length. In the central region of the MVB is located the Acambay graben an intra-arc tectonic depression structure, of apparent Quaternary age, which gives rise to pronounced scarps over a distance of about 80 Km. and 15 to 35 Km wide. The general arrangement of the faults that constitute the Acambay graben shows E-W trend which defines the fronts of the graben exhibits a major fault discontinuity. The graben is limited of the north by the Acambay- Tixmadeje and Epitafio Huerta faults and in the south by the Pastores and Venta de Bravo faults.. In the northern wall in the graben is located the Amealco caldera. This volcanic center (approximately 10 km in diameter) was formed by several discrete volcanic events, which produced an ignimbrite which covers the area. It is partially cut by a regional fault and the southern portion of the Amealco Caldera was displaced by a normal faulting along a segment of the Epitafio Huerta system. Continued tectonic activity in the Acambay area is confirmed by recent seismic episodes The Amealco tuff is the most important volcanic unit because of its volume and distribution. Aeromagnetic data was obtained and analyzed the anomalies. The anomaly map was compared with the surface geology and larger anomalies were correlated with major volcanic features. Since our main interest was in mapping the subsurface intrusive and volcanic bodies, the total field magnetic anomalies were reduced to the pole by using the double integral Fourier method. The reduced to the pole anomaly map results in a simplified pattern of isolated positive and negative anomalies, which show an improved correlation with all major volcanic structures. For the analysis and interpretation of the anomalies, the reduced to the pole anomalies were continued upward at various reference levels. These operations result in smoothing of the anomaly field by

Spatial b-value variations in the Upper Rhine Graben

Science.gov (United States)

Barth, A.

2012-04-01

The natural seismicity of the Upper Rhine Graben (URG) is of growing interest for science and society, since the management of deep geothermal power plants requires local hazard assessment. The availability of new bulletin data and the combination of catalogues from Germany, France and Switzerland allows us to analyse the spatial changes in the magnitude-frequency distribution along the Graben axis in detail. We derive magnitude conversions between the different bulletins to obtain a uniform earthquake catalogue and decluster the data to extract fore- and aftershocks resulting in a Poissonian event distribution. Since the density of monitoring seismometers has improved over time, we determine several intervals of magnitude completeness. Generally, our catalogue is complete for magnitudes ML ≥ 2.0 since 1982 for the entire URG. To incorporate high magnitude events it is essential to use historic earthquake data. Those magnitudes are estimated by their macroseismic intensity distribution, and thus, they have a high uncertainty compared to instrumental magnitudes. We show that historic earthquake magnitudes are overestimated by 0.4 magnitude units in the URG. We apply a spatial window on the final dataset and move it along the Graben axis. For each set of 50 events we determine local variations of the magnitude frequency distribution after Gutenberg-Richter by a maximum likelihood estimation. The seismicity rate for ML ≥ 2.0 varies between 2 per year per 1000 km2 in the southern URG and 0.2 per year per 1000 km2 in the northern URG. The b-values vary between 0.8 and 1.4 with the highest values around Freiburg, showing a high variability of the magnitude distribution in the URG. Additionally, we examine the hypocentral depth distribution along the Graben, which results in a seismically active upper and lower crust in the southern and northern parts, separated by the central part with missing seismicity in the lower crust. According to the spatial distribution of b

Graben structure in the Las Cañadas edifice (Tenerife, Canary Islands): implications for active degassing and insights on the caldera formation

Science.gov (United States)

Galindo, Inés; Soriano, Carles; Martí, Joan; Pérez, Nemesio

2005-06-01

A graben structure has been identified at the western area of the Las Cañadas caldera wall, here referred as the Los Azulejos Graben. This graben is 1 km wide and is bounded by two major normal faults trending NE-SW, the Los Azulejos Fault and the Ucanca Fault. The graben was active for at least 0.5 Ma, from the end of the Ucanca Fm to the end of the Guajara Fm, and before the collapse of the Las Cañadas edifice that formed the western caldera. A right-lateral transtension regime operated in the graben as suggested by small fault orientations and kinematics. The prolongation of the NE rift zone of Tenerife to the Cañadas edifice is the most likely volcano-tectonic scenario for the graben. In this context, inflation of phonolitic shallow magma chambers may have produced reverse faults and reactivation of normal faults. An intense and widespread hydrothermal alteration, here called Azulejos-type, occurred mainly before the graben formation, while a fault-related hydrothermal alteration occurred during and after the graben. Diffuse carbon dioxide and hydrogen degassing in and around the Las Cañadas caldera show relatively enriched values along a NE-SW trend suggesting that faults in the Los Azulejos Graben act as a pathway for deep-seated gases to the surface. Diffuse degassing and hydrothermalism indicate that the graben area has been a zone of intense fluid circulation during the evolution of the Las Cañadas edifice.

Back-arc basalts from the Loncopue graben (Province of Neuquen, Argentina)

Science.gov (United States)

Varekamp, J. C.; Hesse, A.; Mandeville, C. W.

2010-11-01

Young basaltic back-arc volcanoes occur east of the main Andes chain at about 37.5°-39°S in the Loncopue graben, Province of Neuquen, Argentina. These olivine-rich basalts and trachybasalts have up to 8% MgO, with high Ni and Cr contents, but highly variable incompatible element concentrations. Mafic lava flows and cinder cones at the southern end of the graben lack phenocrystic plagioclase. The northern samples have relative Ta-Nb depletions and K, Pb and LREE enrichment. These samples strongly resemble rocks of the nearby arc volcanoes Copahue and Caviahue, including their Fe-Ti enrichment relative to the main Andes arc rocks. The Sr, Nd and Pb isotope ratios show that the source regions of these back-arc basalts are enriched in subducted components that were depleted in the aqueous mobile elements such as Cs, Sr and Ba as a result of prior extractions from the subducted complex below the main arc. Some mafic flows show slightly low 206Pb/ 204Pb and 143Nd/ 144Nd values as well as incompatible trace element ratios similar to southern Patagonia plateau back-arc basalts, suggesting contributions from an EM1 mantle source. Geothermometry and barometry suggest that the basalts crystallized and fractionated small amounts of olivine and spinel at ˜ 35 km depth at temperatures of 1170-1220 °C, at about QFM + 0.5 to QFM + 1 with 1-2% H 2O, and then rose rapidly to the surface. The Loncopue graben back-arc basalts are transitional in composition between the South Patagonia back-arc plateau basalts and the Caviahue and Copahue arc volcanoes to the northwest. The EM1 source endmember is possibly the subcontinental lithospheric mantle. Strong variations in incompatible element enrichment and isotopic compositions between closely spaced cinder cones and lava flows suggest a heterogeneous mantle source for the Loncopue graben volcanics.

Tectonic Geomorphology of the northern Upper Rhine Graben, Germany.

NARCIS (Netherlands)

Peters, G; van Balen, R.T.

2007-01-01

This paper focuses on the northern Upper Rhine Graben (URG), which experienced low tectonic deformation and multiple climate changes during Quaternary times. Recently, human modifications have been high. The paper presents the results of a study into the effects of fault activity on the landscape

Preliminary Geologic Map of the Vermejo Peak area, Colfax and Taos Counties, New Mexico and Las Animas and Costilla Counties, Colorado

Science.gov (United States)

Fridrich, Christopher J.; Shroba, Ralph R.; Pillmore, Charles L.; Hudson, Adam M.

2009-01-01

This geologic map covers four 7.5-minute quadrangles-The Wall, NM-CO (New Mexico-Colorado), Vermejo Park, NM-CO, Ash Mountain, NM, and Van Bremmer Park, NM. The study area straddles the boundary between the eastern flank of the Sangre de Cristo Mountains and the western margin of the Raton Basin, with about two-thirds of the map area in the basin. The Raton Basin is a foreland basin that formed immediately eastward of the Sangre de Cristo Mountains during their initial uplift, in the Late Cretaceous through early Eocene Laramide orogeny. Subsequently, these mountains have been extensively modified during formation of the Rio Grande rift, from late Oligocene to present. The map area is within that part of the Sangre de Cristo Mountains that is called the Culebra Range. Additionally, the map covers small parts of the Devil's Park graben and the Valle Vidal half-graben, in the northwestern and southwestern parts of the map area, respectively. These two grabens are small intermontaine basins, that are satellitic to the main local basin of the Rio Grande rift, the San Luis Basin, that are an outlying, early- formed part of the rift, and that separate the Culebra Range from the Taos Range, to the southwest.

Implications of horsts and grabens on the development of canyons and seismicity on the west africa coast

Science.gov (United States)

Ola, Peter S.; Olabode, Solomon O.

2018-04-01

Subsurface basement topography in the Nigerian portion of the Benin Basin has been studied using borehole data of wells drilled to the basement and one strike line of seismic section. Two areas of a sharp drop in topography with a horst in between were observed in the study area. These features were projected to a seismic section in the offshore area of the Benin basin. The result depicts the structural features as horst and grabens coinciding with the Avon platform bounded on the right side by Ise graben, and the Orimedu graben to the left. The observed relationship of the grabens with the present day location of Avon Canyon on the seismic section also suggests an active subsidence along fractured zones. The subsidence, which probably is occurring along similar fracture zones in the Gulf of Guinea, could be responsible for the occasionally reported seismicity on the margin of West Africa. A detailed seismographic study of the fracture zones is recommended.

VALLE DE ABURRÁ: ¿QUO VADIS?

Directory of Open Access Journals (Sweden)

Hermelin Michel

2008-07-01

Full Text Available Se da una descripción somera de la evolución que ha tenido la prevención de los riesgos de origen natural en el Valle de Aburrá . Tanto la naturaleza litológica y estructural del valle como sus condiciones topográficas y climáticas lo hacen propenso a la ocurrencia de fenómenos naturales como sismos, movimientos de vertiente, avenidas torrenciales y, en menor grado, inundaciones. El aumento de la población que es actualmente de 3.5 millones de habitantes y la frecuente ocupación de lugares expuestos a amenazas han resultado en numerosos desastres. En este momento funcionan para la prevención y atención de desastres entidades como el SIMPAD y el DAPARD, con responsabilidades municipales y departamentales respectivamente. El grado de conocimiento del entorno físico del valle se considera insuficiente, así como las reglamentaciones que deberían tener como consecuencias de un uso de la tierra más acorde con las restricciones naturales. Se han realizado ya varias reuniones acerca de la gestión de riesgos naturales en la zona y los organizadores de la de 2007, que conmemora el vigésimo aniversario de la catástrofe de Villa Tina, pueden tomar la decisión de llevarlas a cabo cada dos años. Asimismo proponen la creación de un grupo técnicocientífico permanente dispuesto a estudiar los eventos ocurridos, a fomentar la difusión de la información pertinente y en general a propender por un mejor conocimiento del Valle de Aburrá.

el Valle del Cauca

Directory of Open Access Journals (Sweden)

Carlos Humberto Ortiz

2007-01-01

Full Text Available Este artículo se enfoca en la identi- ficación de aquellos factores estructurales que explican la pérdida de dinamismo económico de largo plazo en Colombia y, en particular, en el Valle del Cauca. Se examina la competitividad del Valle en relación con Colombia y con el resto del mundo. Se cuestiona la insistencia en una estrategia exportadora como dinamizadora del desarrollo económico. Se identifica que una gran parte de la población está excluida de los beneficios del desarrollo económico. Para construir un modelo de desarrollo que incluya a esta población se recomienda recuperar la senda de la industrialización, invertir en el capital humano (educación de alta calidad, salud, salubridad y nutrición, e invertir en infraestructura. La participación del Estado en estas inversiones sociales es necesaria para disminuir la desigualdad y aumentar el crecimiento económico.

Chapter 1. Valles Caldera National Preserve land use history

Science.gov (United States)

Kurt F. Anschuetz

2007-01-01

The land use history of the Valles Caldera National Preserve (VCNP) extends back over thousands of years. Few known archaeological properties in the Valles Caldera date to the Paleoindian period (10000/9500–5500 B.C.). These finds include the recent discovery, during ongoing archaeological studies (Dr. Bob Parmeter, personal communication, VCNP, Los Alamos, 2005), of...

Gigantism in tadpoles of the Neogene frog Palaeobatrachus

Czech Academy of Sciences Publication Activity Database

Roček, Zbyněk; Böttcher, R.; Wassersug, R.

2006-01-01

Roč. 32, č. 4 (2006), s. 666-675 ISSN 0094-8373 R&D Projects: GA AV ČR IAA3013206 Institutional research plan: CEZ:AV0Z30130516 Keywords : Amphibia * Anura * Neogene * Germany * development Subject RIV: EG - Zoology Impact factor: 2.405, year: 2006

Cacilda Borges Do Valle

Indian Academy of Sciences (India)

Home; Journals; Journal of Genetics. Cacilda Borges Do Valle. Articles written in Journal of Genetics. Volume 83 Issue 3 December 2004 pp 279-283 Research Note. Abnormal pollen mitoses (PM I and PM II) in an interspecific hybrid of Brachiaria ruziziensis and Brachiaria decumbens (Gramineae) · Andréa Beatriz ...

Neogene climate evolution in Amazonia and the Brazilian Northeast

NARCIS (Netherlands)

Hoorn, C.; Bernardes-de-Oliveira, M.E.C.; Dino, R.; Garcia, M.J.; Antonioli, L.; da Costa Casado, F.; Hooghiemstra, H.; de Souza Carvalho, I.; Garcia, M.J.; Strohschoen, O.; Cunha Lana, C.

2014-01-01

Climate change follows from the interaction between global atmospheric and oceanic processes with regional processes. In this chapter we review which factors determined climate evolution in Amazonia and the Brazilian Northeast and present a recompilation of Neogene palynological and paleobotanical

Multi-scale, multi-method geophysical investigations of the Valles Caldera

Science.gov (United States)

Barker, J. E.; Daneshvar, S.; Langhans, A.; Okorie, C.; Parapuzha, A.; Perez, N.; Turner, A.; Smith, E.; Carchedi, C. J. W.; Creighton, A.; Folsom, M.; Bedrosian, P.; Pellerin, L.; Feucht, D. W.; Kelly, S.; Ferguson, J. F.; McPhee, D.

2017-12-01

In 2016, the Summer of Applied Geophysical Experience (SAGE) program, in cooperation with the National Park Service, began a multi-year investigation into the structure and evolution of the Valles Caldera in northern New Mexico. The Valles Caldera is a 20-km wide topographic depression in the Jemez Mountains volcanic complex that formed during two massive ignimbrite eruptions at 1.65 and 1.26 Ma. Post-collapse volcanic activity in the caldera includes the rise of Redondo peak, a 1 km high resurgent dome, periodic eruptions of the Valles rhyolite along an inferred ring fracture zone, and the presence of a geothermal reservoir beneath the western caldera with temperatures in excess of 300°C at a mere 2 km depth. Broad sediment-filled valleys associated with lava-dammed Pleistocene lakes occupy much of the northern and southeastern caldera. SAGE activities to date have included collection of new gravity data (>120 stations) throughout the caldera, a transient electromagnetic (TEM) survey of Valle Grande, reprocessing of industrial magnetotelluric (MT) data collected in the 1980s, and new MT data collection both within and outside of the caldera. Gravity modeling provides constraints on the pre-Caldera structure, estimates of the thickness of Caldera fill, and reveals regional structural trends reflected in the geometry of post-Caldera collapse. At a more local scale, TEM-derived resistivity models image rhyolite flows radiating outward from nearby vents into the lacustrine sediments filling Valle Grande. Resistivity models along a 6-km long profile also provide hints of structural dismemberment along the inferred Valles and Toledo ring fracture zones. Preliminary MT modeling at the caldera scale reveals conductive caldera fill, the resistive crystalline basement, and an enigmatic mid-crustal conductor likely related to magmatic activity that post-dates caldera formation.

Is Kasei Valles (Mars) the largest volcanic channel in the solar system?

Science.gov (United States)

Leverington, David W.

2018-02-01

With a length of more than 2000 km and widths of up to several hundred kilometers, Kasei Valles is the largest outflow system on Mars. Superficially, the scabland-like character of Kasei Valles is evocative of terrestrial systems carved by catastrophic aqueous floods, and the system is widely interpreted as a product of outbursts from aquifers. However, as at other Martian outflow channels, clear examples of fluvial sedimentary deposits have proven difficult to identify here. Though Kasei Valles lacks several key properties expected of aqueous systems, its basic morphological and contextual properties are aligned with those of ancient volcanic channels on Venus, the Moon, Mercury, and Earth. There is abundant evidence that voluminous effusions of low-viscosity magmas occurred at the head of Kasei Valles, the channel system acted as a conduit for associated flows, and mare-style volcanic plains developed within its terminal basin. Combined mechanical and thermal incision rates of at least several meters per day are estimated to have been readily achieved at Kasei Valles by 20-m-deep magmas flowing with viscosities of 1 Pa s across low topographic slopes underlain by bedrock. If Kasei Valles formed through incision by magma, it would be the largest known volcanic channel in the solar system. The total volume of magma erupted at Kasei Valles is estimated here to have possibly reached or exceeded ∼5 × 106 km3, a volume comparable in magnitude to those that characterize individual Large Igneous Provinces on Earth. Development of other large outflow systems on Mars is expected to have similarly involved eruption of up to millions of cubic kilometers of magma.

Valle del Chota: fútbol, identidad y mercado

OpenAIRE

Ortiz Villalva, Verónica

2011-01-01

Al fútbol se le ha conferido varios sentidos y valor social: juego, deporte, ritual, opio, espectáculo, negocio, etc. Cada faceta responde a la apropiación que los grupos sociales han hecho de este deporte. En este sentido, podríamos decir que el fútbol también significa movilidad socioeconómica, inclusión real y simbólica, reconocimiento y visibilización, al menos, para el Valle del Chota. El Valle del Chota, conocido como la cantera de los mejores futbolistas del país, es ...

Los tambos Inca: el caso de Camata Tambo valle alto de Moquegua

OpenAIRE

Chacaltana Cortez, Sofía; Ministerio de Cultura

2013-01-01

Camata Tambo está ubicado en la parte alta del valle alto de Moquegua. Por este tambo pasa un camino Inca que viene del altiplano y continúa hacia el centro provincial de Sabaya ubicado a 1 km valle abajo.

Use of deep seismic shooting to study graben-like troughs. [Urals

Energy Technology Data Exchange (ETDEWEB)

Makalovskiy, V.V.; Silayev, V.A.

1983-01-01

In the Southeast Perm Oblast, in the zone of articulation of the Russian platform and the Cisural trough, in order to study the structure of the graben-like troughs together with deep drilling, well seismic exploration is used by the method of deep seismic shooting (DSS). The DSS method developed by the Kamskiy department of the VNIGNI consists of blasting in the well shaft and recording of the elastic fluctuations on the Earth's surface. The use of the DSS made it possible to pinpoint structural details of the graben-like trough, and to clarify that this is in essence a zone of fracturing, where the lowered blocks alternated with elevated, and to establish the location and amplitude of the tectonic disorders. High geological information content, low labor intensity and rapidity of obtaining the results make it possible to recommend the DSS together with prospecting and exploratory drilling to study complexly constructed objects in order to reduce the number of unproductive wells.

Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)

Science.gov (United States)

Ferraro, Serena; Sulli, Attilio; Di Stefano, Enrico; Giaramita, Luigi; Incarbona, Alessandro; Graham Mortyn, P.; Sprovieri, Mario; Sprovieri, Rodolfo; Tonielli, Renato; Vallefuoco, Mattia; Zizzo, Elisabetta; Tranchida, Giorgio

2018-03-01

The Malta Graben is a deep tectonic depression in the Sicily Channel, bounded by NW-SE normal faults and filled by thick Pliocene-Quaternary deposits. A previous analysis of a giant piston core (LC09) from the Malta Graben had revealed a wide range of sedimentary features (carbonate turbidites, bioturbated mud and scours), although the chronostratigraphic constraint of the stacking pattern has remained elusive. After establishing a reliable chronological framework based on seven radiocarbon dates for a shorter core from the Malta Graben (ANSIC03-735), a down-core analysis of planktonic foraminifer and coccolith abundance, stable isotopes and sediment grain size was carried out. Since the last glacial maximum, palaeoenvironmental conditions (surface fertility and deep chlorophyll maximum during the last glacial and the Younger Dryas; warm and oligotrophic water masses, with a deep nutricline and intense winter mixing during the Holocene) as well as selected calcareous plankton taxa trends and peaks seem to be similar to those reported for other central and western Mediterranean sites, possibly in spite of a unique response of these areas to late Quaternary climatic fluctuations. Four distinct layers, each tens of centimetres thick, are barren of foraminifers but not of coccoliths. Morphobathymetric data as well as new high-resolution and high-penetration seismic profiles show that prolonged contouritic activity has persisted on the western side of the Malta Graben. It is thus likely that layers barren of foraminifers are due to the overflow of fine-grained (clayey) material beyond drift channel dikes.

Late Quaternary palaeoenvironmental reconstruction of sediment drift accumulation in the Malta Graben (central Mediterranean Sea)

Science.gov (United States)

Ferraro, Serena; Sulli, Attilio; Di Stefano, Enrico; Giaramita, Luigi; Incarbona, Alessandro; Graham Mortyn, P.; Sprovieri, Mario; Sprovieri, Rodolfo; Tonielli, Renato; Vallefuoco, Mattia; Zizzo, Elisabetta; Tranchida, Giorgio

2018-06-01

The Malta Graben is a deep tectonic depression in the Sicily Channel, bounded by NW-SE normal faults and filled by thick Pliocene-Quaternary deposits. A previous analysis of a giant piston core (LC09) from the Malta Graben had revealed a wide range of sedimentary features (carbonate turbidites, bioturbated mud and scours), although the chronostratigraphic constraint of the stacking pattern has remained elusive. After establishing a reliable chronological framework based on seven radiocarbon dates for a shorter core from the Malta Graben (ANSIC03-735), a down-core analysis of planktonic foraminifer and coccolith abundance, stable isotopes and sediment grain size was carried out. Since the last glacial maximum, palaeoenvironmental conditions (surface fertility and deep chlorophyll maximum during the last glacial and the Younger Dryas; warm and oligotrophic water masses, with a deep nutricline and intense winter mixing during the Holocene) as well as selected calcareous plankton taxa trends and peaks seem to be similar to those reported for other central and western Mediterranean sites, possibly in spite of a unique response of these areas to late Quaternary climatic fluctuations. Four distinct layers, each tens of centimetres thick, are barren of foraminifers but not of coccoliths. Morphobathymetric data as well as new high-resolution and high-penetration seismic profiles show that prolonged contouritic activity has persisted on the western side of the Malta Graben. It is thus likely that layers barren of foraminifers are due to the overflow of fine-grained (clayey) material beyond drift channel dikes.

Gravitational collapse and Neogene sediment transfer across the western margin of the Gulf of Mexico: Insights from numerical models

NARCIS (Netherlands)

Alzaga-Ruiz, H.; Granjeon, D.; Lopez, M.; Séranne, M.; Roure, F.

2009-01-01

The western margin of the Gulf of Mexico (Veracruz State, Mexico) displays an extensive Neogene gravitational system, whereby the Neogene siliciclastic sediments are detached from underlying Mesozoic carbonates along decollement surface in Oligocene underpressured clays. Rapidly subsiding

Maja Valles, Mars: A Multi-Source Fluvio-Volcanic Outflow Channel System

Science.gov (United States)

Keske, A.; Christensen, P. R.

2017-12-01

The resemblance of martian outflow channels to the channeled scablands of the Pacific Northwest has led to general consensus that they were eroded by large-scale flooding. However, the observation that many of these channels are coated in lava issuing from the same source as the water source has motivated the alternative hypothesis that the channels were carved by fluid, turbulent lava. Maja Valles is a circum-Chryse outflow channel whose origin was placed in the late Hesperian by Baker and Kochel (1979), with more recent studies of crater density variations suggesting that its formation history involved multiple resurfacing events (Chapman et al., 2003). In this study, we have found that while Maja Valles indeed host a suite of standard fluvial landforms, its northern portion is thinly coated with lava that has buried much of the older channel landforms and overprinted them with effusive flow features, such as polygons and bathtub rings. Adjacent to crater pedestals and streamlined islands are patches of dark, relatively pristine material pooled in local topographic lows that we have interpreted as ponds of lava remaining from one or more fluid lava flows that flooded the channel system and subsequently drained, leaving marks of the local lava high stand. Despite the presence of fluvial landforms throughout the valles, lava flow features exist in the northern reaches of the system alone, 500-1200 km from the channels' source. The flows can instead be traced to a collection of vents in Lunae Plaum, west of the valles. In previously studied fluvio-volcanic outflow systems, such as Athabasca Valles, the sources of the volcanic activity and fluvial activity have been indistinguishable. In contrast, Maja Valles features numerous fluvio-volcanic landforms bearing similarity to those identified in other channel systems, yet the source of its lava flows is distinct from the source of its channels. Furthermore, in the absence of any channels between the source of the lava

Application of helium isotopes in shallow groundwaters for geothermal energy exploration in the Upper Rhine Graben

International Nuclear Information System (INIS)

Freundt, Florian

2017-01-01

The helium isotope system is an established tool in hydrology for identifying mantle fluids in deep aquifers. This study applies the helium tracer system for the first time in shallow, unconfined aquifers of the Upper Rhine Graben. The Graben is a part of the Cenozoic Rift system of Western and Central Europe, a continental rift zone with unusually high geothermal gradients, making it an ideal region of Germany for geothermal energy development. The aim of this study is to develop a suite of natural groundwater tracers able to achieve a cost and effort reduction in geothermal prospection. The 3 He/ 4 He-ratio is therefore applied, as part of a multi-tracer approach including 3 H, δ 18 O, δ 2 H, δ 13 C, 14 C and 222 Rn, to identify and locate fault zones with suitable permeabilities for power plant operation. Three target areas along the graben were studied, each located on one of the main fault lines. A mantle-derived helium signature could be identified and separated from tritiogenic helium in a shallow aquifer in the north-west of the Graben. The mixing component of mantle-derived fluid in the shallow groundwater is calculated to reach up to 5%, based on the analysis of the 3 He/ 4 He isotope system. The employed method proves that the local permeability of the fault zone is high. The origin of the locally occurring upwelling of salinated water can be redetermined by the data.

Active deformation in the northern Sierra de Valle Fértil, Sierras Pampeanas, Argentina

Science.gov (United States)

Ortiz, Gustavo; Alvarado, Patricia; Fosdick, Julie C.; Perucca, Laura; Saez, Mauro; Venerdini, Agostina

2015-12-01

The Western Sierras Pampeanas region in the San Juan Province is characterized by thick-skinned deformation with approximately N-S trending ranges of average heights of 2500 m and a high frequency occurrence of seismic activity. Its location to the east of the mainly thin-skinned tectonics of the Argentine Precordillera fold-and-thrust belt suggests that at 30°S, deformation is concentrated in a narrow zone involving these two morphostructural units. In this paper, we present new apatite (U-Th)/He results (AHe) across the northern part of the Sierra de Valle Fértil (around 30°S) and analyze them in a framework of thermochronologic available datasets. We found Pliocene AHe results for Carboniferous and Triassic strata in the northern Sierra de Valle Fértil consistent with the hypothesis of recent cooling and inferred erosional denudation concentrated along the northern end of this mountain range. Our analysis shows that this northern region may have evolved under different conditions than the central part of the Sierra de Valle Fértil. Previous studies have observed AHe ages consistent with Permian through Cretaceous cooling, indicating the middle part of the Sierra de Valle Fértil remained near surface before the Pampean slab subduction flattening process. Those studies also obtained ˜5 My cooling ages in the southern part of the Sierra de Valle Fértil, which are similar to our results in the northern end of the range. Taken together, these results suggest a pattern of young deformation in the northern and southern low elevation ends of the Sierra de Valle Fértil consistent with regions of high seismic activity, and Quaternary active faulting along the western-bounding thrust fault of the Sierra de Valle Fértil.

Application of helium isotopes in shallow groundwaters for geothermal energy exploration in the Upper Rhine Graben

Energy Technology Data Exchange (ETDEWEB)

Freundt, Florian

2017-07-12

The helium isotope system is an established tool in hydrology for identifying mantle fluids in deep aquifers. This study applies the helium tracer system for the first time in shallow, unconfined aquifers of the Upper Rhine Graben. The Graben is a part of the Cenozoic Rift system of Western and Central Europe, a continental rift zone with unusually high geothermal gradients, making it an ideal region of Germany for geothermal energy development. The aim of this study is to develop a suite of natural groundwater tracers able to achieve a cost and effort reduction in geothermal prospection. The {sup 3}He/{sup 4}He-ratio is therefore applied, as part of a multi-tracer approach including {sup 3}H, δ{sup 18}O, δ{sup 2}H, δ{sup 13}C, {sup 14}C and {sup 222}Rn, to identify and locate fault zones with suitable permeabilities for power plant operation. Three target areas along the graben were studied, each located on one of the main fault lines. A mantle-derived helium signature could be identified and separated from tritiogenic helium in a shallow aquifer in the north-west of the Graben. The mixing component of mantle-derived fluid in the shallow groundwater is calculated to reach up to 5%, based on the analysis of the {sup 3}He/{sup 4}He isotope system. The employed method proves that the local permeability of the fault zone is high. The origin of the locally occurring upwelling of salinated water can be redetermined by the data.

CARACTERIZACIÓN COLORIMÉTRICA DEL MANJAR BLANCO DEL VALLE CARACTERIZAÇÃO COLORIMÉTRICA DE MANJAR BRANCO DEL VALLE COLORIMETRIC CHARACTERIZATION OF MANJAR BLANCO DEL VALLE

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DIEGO FABIÁN NOVOA

2012-12-01

Full Text Available El Manjar Blanco del Valle originario de la región del Valle del Cauca en Colombia es considerado como símbolo gastronómico y cultural; es un tipo de dulce de leche con adición de almidón. El color es uno de los atributos más importantes en los alimentos. La medición del color tiene aplicaciones en el control de calidad y el desarrollo de nuevos productos. En esta investigación se caracteriza el color instrumental (escala CIE-L*a*b* del manjar blanco del Valle elaborado por empresas representativas y tradicionales de la región, mediante la determinación de los parámetros de color (L*, a*, b* de tres lotes de cada una de las marcas comerciales. También se caracterizó físicamente las muestras, encontrando pH entre 5,73 y 6,02 y grados Brix entre 65,16 y 76,47. Los valores promedio de los parámetros de color determinados experimentalmente para el manjar blanco fueron: L* 43,60, a* 14,58 y b* 34,67. De los datos reportados en este trabajo se concluye que existe una variabilidad considerable en el color entre lotes y marcas comerciales, lo que evidencia la necesidad de establecer procedimientos de estandarización en la producción y en la materia prima, con el fin de lograr un producto con características similares.O Manjar Branco Del Valle originário da região do Vale de Cauca na Colômbia é considerado um símbolo gastronômico e cultural; é um tipo de doce de leite com adição de amido. A coloração é um dos atributos mais importantes nos alimentos. A determinação da cor tem aplicações no controle de qualidade e no desenvolvimento de novos produtos. Neste estudo se caracterizou a cor instrumental (Sistema CIE-L*a*b* do Manjar Branco Del Valle produzido por empresas representativas e tradicionais da região, mediante a determinação dos parâmetros de cor (L*, a*, b* de três lotes de cada uma das marcas comerciais. Também se caracterizou fisicamente as amostras, encontrando pH entre 5,73 e 6,02 e graus Brix entre 65

Assessment of Late Quaternary strain partitioning in the Afar Triple Junction: Dobe and Hanle grabens, Ethiopia and Djibouti

Science.gov (United States)

Polun, S. G.; Stockman, M. B.; Hickcox, K.; Horrell, D.; Tesfaye, S.; Gomez, F. G.

2015-12-01

As the only subaerial exposure of a ridge - ridge - ridge triple junction, the Afar region of Ethiopia and Djibouti offers a rare opportunity to assess strain partitioning within this type of triple junction. Here, the plate boundaries do not link discretely, but rather the East African rift meets the Red Sea and Gulf of Aden rifts in a zone of diffuse normal faulting characterized by a lack of magmatic activity, referred to as the central Afar. An initial assessment of Late Quaternary strain partitioning is based on faulted landforms in the Dobe - Hanle graben system in Ethiopia and Djibouti. These two extensional basins are connected by an imbricated accommodation zone. Several fault scarps occur within terraces formed during the last highstand of Lake Dobe, around 5 ka - they provide a means of calibrating a numerical model of fault scarp degradation. Additional timing constraints will be provided by pending exposure ages. The spreading rates of both grabens are equivalent, however in Dobe graben, extension is partitioned 2:1 between northern, south dipping faults and the southern, north dipping fault. Extension in Hanle graben is primarily focused on the north dipping Hanle fault. On the north margin of Dobe graben, the boundary fault bifurcates, where the basin-bordering fault displays a significantly higher modeled uplift rate than the more distal fault, suggesting a basinward propagation of faulting. On the southern Dobe fault, surveyed fault scarps have ages ranging from 30 - 5 ka with uplift rates of 0.71, 0.47, and 0.68 mm/yr, suggesting no secular variation in slip rates from the late Plestocene through the Holocene. These rates are converted into horizontal stretching estimates, which are compared with regional strain estimated from velocities of relatively sparse GPS data.

Aportaciones al conocimiento de la compresión tardía en la Cordillera Ibérica centro-oriental: la cuenca neógena inferior del Mijares (Teruel-Castellón

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Paricio Cardona, J.

1986-10-01

Full Text Available The lower Neogene deposits of the Mijares valley (mainly fluvial facies are filling three paralell• grabens controlled by synsedimentary ENE normal faults. This structural pattern is created during a moderate compression phase with an ENE horizontal σ₁ axis which sometimes can be permuted with the vertical σ₂. Afterwards. a second SSE to S compression affects these deposits. The age of the basin can be established in the Upper Aragonian-Lower Vallesian bested on the Micromamal fauna found in two localities. Other sites in the cetral-oriental lberian Chain also show compressive deformations in well-dated deposits of Agenian and Aragonian ages. The compression still continues in this region during the Lower and Middle Miocene, the passage to the extension regime talking place in the Vanesian.

Las facies esencialmente fluviales que integran la unidad interior~ del valle medio del Mijares se depositan en tres grabens paralelos controlados por fallas sinsedimentarias ENE de componente normal. Este dispositivo estructural se crea en el curso de una etapa. compresiva de intensidad moderada, con un σ₁ según ENE, que eventualmente se intercambia con σ₂ vertical. Una segunda etapa de compresión SSE a S afecta posteriormente a esta unidad, datada en el Astaranciense-Vallesiense gracias a la fauna de micromamíferos proporcionada por dos yacimientos. Otras localidades de la Cadena Ibérica centro-oriental registran asimismo deformaciones compresivas en depósitos bien datados entre el Ageniense y el Aragoniense. Aunque sin producir apenas pliegues, el régimen compresivo perdura aún claramente en este sector de la cadena durante toda la primera mitad del Mioceno, siendo en el Vallesiense cuando se produce el tránsito definitivo a la distensión.

Geomorphological and structural characterization of the southern Weihe Graben, central China: Implications for fault segmentation

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Cheng, Yali; He, Chuanqi; Rao, Gang; Yan, Bing; Lin, Aiming; Hu, Jianmin; Yu, Yangli; Yao, Qi

2018-01-01

The Cenozoic graben systems around the tectonically stable Ordos Block, central China, have been considered as ideal places for investigating active deformation within continental rifts, such as the Weihe Graben at the southern margin with high historical seismicity (e.g., 1556 M 8.5 Huaxian great earthquake). However, previous investigations have mostly focused on the active structures in the eastern and northern parts of this graben. By contrast, in the southwest, tectonic activity along the northern margin of the Qinling Mountains has not been systematically investigated yet. In this study, based on digital elevation models (DEMs), we carried out geomorphological analysis to evaluate the relative tectonic activity along the whole South Border Fault (SBF). On the basis of field observations, high resolution DEMs acquired by small unmanned aerial vehicles (sUVA) using structure-for-motion techniques, radiocarbon (14C) age dating, we demonstrate that: 1) Tectonic activity along the SBF changes along strike, being higher in the eastern sector. 2) Seven major segment boundaries have been assigned, where the fault changes its strike and has lower tectonic activity. 3) The fault segment between the cities of Huaxian and Huayin characterized by almost pure normal slip has been active during the Holocene. We suggest that these findings would provide a basis for further investigating on the seismic risk in densely-populated Weihe Graben. Table S2. The values and classification of geomorphic indices obtained in this study. Fig. S1. Morphological features of the stream long profiles (Nos. 1-75) and corresponding SLK values. Fig. S2. Comparison of geomorphological parameters acquired from different DEMs (90-m SRTM and 30-m ASTER GDEM): (a) HI values; (b) HI linear regression; (c) mean slope of drainage basin; (d) mean slope linear regression.

Radionuclide transport in the Neogene aquifer system located in the environment of the Boom clay

International Nuclear Information System (INIS)

Gedeon, M.; Marivoet, J.; Vandersteen, K.

2012-01-01

Document available in extended abstract form only. In the framework the Belgian research program on the long term management of high-level and/or long-lived radioactive waste coordinated by ONDRAF/NIRAS, the Boom Clay is considered as a reference host rock for the geological disposal of high-level radioactive waste in NE-Belgium (Campine area). In the frame of the performance assessments of a disposal system located in the Boom Clay Formation, the transport of radionuclides diffusing through the clay barrier into the aquifers located above is modelled. The transport model for the Neogene aquifer is based on a series of groundwater flow models simulating the aquifer systems in the surroundings of the Boom Clay. This series of groundwater models include the regional north-eastern Belgium model simulating flow both above and below the Boom Clay, the recently updated deep-aquifer pumping model, simulating transient flow in the over-exploited aquifers below the Boom Clay and finally the catchment-scale Neogene aquifer model, simulating flow in the aquifer system above the Boom Clay. The Neogene aquifer system consists of two main aquifers. The Pliocene aquifer is located at the top, separated from the underlying Miocene aquifer by the Kasterlee Clay aquitard. The Miocene aquifer consists of three hydrostratigraphic units: the Diest, Berchem and Voort Formations; with the last two having a lower hydraulic conductivity than the Diest unit. The transport model for the Neogene aquifer represents a fraction of the catchment-scale Neogene aquifer model. It stretches from the local divide between the Grote and Kleine Nete Rivers up to the Kleine Nete River, representing the main model sink. The boundary conditions and the sources/sinks in the Pliocene aquifer are defined mostly by the surface water features, such as the rivers, brooks, lakes and canals. In the partially confined Miocene aquifer, the effect of the surface water features is dampened and the heads at the model

Structural and functional analysis of validoxylamine A 7'-phosphate synthase ValL involved in validamycin A biosynthesis.

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Lina Zheng

Full Text Available Validamycin A (Val-A is an effective antifungal agent widely used in Asian countries as crop protectant. Validoxylamine A, the core structure and intermediate of Val-A, consists of two C(7-cyclitol units connected by a rare C-N bond. In the Val-A biosynthetic gene cluster in Streptomyces hygroscopicus 5008, the ORF valL was initially annotated as a validoxylamine A 7'-phosphate(V7P synthase, whose encoded 497-aa protein shows high similarity with trehalose 6-phosphate(T6P synthase. Gene inactivation of valL abolished both validoxylamine A and validamycin A productivity, and complementation with a cloned valL recovered 10% production of the wild-type in the mutant, indicating the involvement of ValL in validoxylamine A biosynthesis. Also we determined the structures of ValL and ValL/trehalose complex. The structural data indicates that ValL adopts the typical fold of GT-B protein family, featuring two Rossmann-fold domains and an active site at domain junction. The residues in the active site are arranged in a manner homologous to that of Escherichia coli (E.coli T6P synthase OtsA. However, a significant discrepancy is found in the active-site loop region. Also noticeable structural variance is found around the active site entrance in the apo ValL structure while the region takes an ordered configuration upon binding of product analog trehalose. Furthermore, the modeling of V7P in the active site of ValL suggests that ValL might have a similar SNi-like mechanism as OtsA.

Late Jurassic rifting in the southern central Graben -A complex story simplified

NARCIS (Netherlands)

Verreussel, R.M.C.H.; Munsterman, D.K.; Ten Veen, J.H.; Weerd, A. van de; Dybkjaer, K.; Johannessen, P.N.

2014-01-01

In order to be able to predict the distribution of reservoir sands and of grainsize and porosity trends in a hydrocarbon province, it is essential to understand the basin evolution in detail. In this study, an attempt is made to reconstruct the complex basin evolution of the southern Central Graben

The Sedimentary History of Southern Central Crete: Implications for Neogene Uplift

Science.gov (United States)

Kröger, K.; Brachert, T. C.; Reuter, M.

2003-04-01

The tectonic setting of Crete was largely extensional since Lower Miocene uplift and exhumation of HP/LT rocks. Erosion of uplifted areas resulted in the deposition of terrestrial to marine sediments in the Messara and Iraclion Basins. There are several concurring models that discuss Late Neogene uplift of the basinal margins. Neogene near shore sediments in the south of the Messara Basin record fault movements contemporaneous to sedimentation and sedimentary input from the hinterland. Therefore they provide information on the paleogeographic situation and the resulting amount of subsidence and uplift of mountain areas since the Upper Miocene. The studied sediments consist of terrestrial to shallow marine, floodplain related sediments of the Upper Miocene Ambelouzos Formation that are overlain by platform limestones of the Upper Miocene Varvara Formation. In the Messara Basin these units are overlain by the Pliocene Kourtes Formation. The stratigraphic architecture of these deposits indicates fragmentation of the basinal margin. Proximal boulder conglomerates and reworked blocks of the Ambelouzos formation indicate fault activity during the deposition of the Varvara Formation. Contents of terrigenous clastics, provided by rivers and distributed by longshore currents, are high in the Ambelouzos and the lower Varvara Formations but decrease rapidly upsection within the Varvara Formation. This indicates drowning of the fault bounded blocks and little topography of the hinterland (Asteroussia Mountains) at that time. The Pliocene marls at the southern margin of the Messara Basin contain lithoclasts of the Upper Miocene limestones and thus indicate uplift of the carbonate platform. The modern topographic elevation of formerly drowned fault bounded blocks requires a minimum uplift of 400m. Main uplift occurred at approximately orthogonal NW-SE and SW-NE striking normal to oblique faults. The present elevation of the Asteroussia Mountains indicates net uplift of at least

Ectopsocidae (Psocodea: 'Psocoptera') from Valle del Cauca and NNP Gorgona, Colombia.

Science.gov (United States)

Manchola, Oscar Fernando Saenz; Obando, Ranulfo González; Aldrete, Alfonso N García

2014-04-14

The results of a survey of the psocid family Ectopsocidae in Valle del Cauca and NNP Gorgona, are here presented. Fifteen species were identified, in the genera Ectopsocus (14 species), and Ectopsocopsis (one species); four of the Ectopsocus species are new to science and are here described and illustrated. The male of E. thorntoni García Aldrete is here described. Records of Ectopsocopsis cryptomeriae (Enderlein), Ectopsocus briggsi McLachlan, E. californicus Banks, E. columbianus Badonnel, E. maindroni Badonnel, E. meridionalis Ribaga, E. pilosus Badonnel, E. richardsi Pearman, E. titschacki Jentsch, and E. vilhenai Badonnel, are provided. Ten species were found only in Valle del Cauca, two species were found only in the NNP Gorgona, and three species were found at both sites. The specimens studied are deposited in the Entomological Museum, Universidad del Valle, Santiago de Cali, Colombia (MUSENUV).

Amazonian volcanism inside Valles Marineris on Mars

Czech Academy of Sciences Publication Activity Database

Brož, Petr; Hauber, E.; Wray, J. J.; Michael, G.

2017-01-01

Roč. 473, September (2017), s. 122-130 ISSN 0012-821X Institutional support: RVO:67985530 Keywords : Mars * Valles Marineris * volcanism * scoria cone * hydrothermal activity Subject RIV: DC - Siesmology, Volcanology, Earth Structure OBOR OECD: Volcanology Impact factor: 4.409, year: 2016

El valle de Mexicali: agricultura e inversión extranjera (1901-1986

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Martha Stamatis Maldonado

1987-01-01

Full Text Available El interés de este trabajo es intentar explicar el desarrollo de la agricultura del valle de Mexicali a través de su relación con la inversión extranjera (norteamericana. Relación que está determinada por la función conformadora del sistema económico internacional representada por el capital norteamericano, la cual se va convirtiendo en un hecho, sobre todo a partir de 1940 en la integración nacional de las actividades económicas y sociales que se desarrollan en México. Este proceso de desarrollo ofrece manifestaciones particulares, la agricultura del valle no está ajena a las determinaciones ejercidas por el capital norteamericano sobre la agricultura nacional. De esta forma, este capital sigue manteniendo su presencia en el valle como parte de la función hegemónica para internacionalizar la agricultura mexicana. Las posibilidades que el valle tiene para un mayor crecimiento estriban en factores que permitirían un mayor desplazamiento de la producción de California, tomando en cuenta la corta distancia, entre otros, para que tuvieran un peso suficiente que las convirtiera en ventajas reales.

Nuevos datos sobre Huaca China, Valle del Santa, Perú

OpenAIRE

Chapdelaine, Claude; Pimentel, Víctor; Gagné, Gérard; Gamboa, Jorge; Regalado, Delicia; Chicoine, David

2015-01-01

La presencia Moche en el valle del Santa se apoya en la existencia de numerosos sitios entre los cuales varios son considerados centros locales de importancia. Huaca China es uno de estos sitios estratégicos en la parte suroeste del valle. Las recolecciones de superficie y la limpieza de pozos de huaquero permiten la identificación de una presencia Moche y de una fuerte ocupación durante el Horizonte Medio. Además de presentar una sepultura de la cultura Tanguche, se describen los principales...

New stratigraphic, chronologic, and magnetic fabric constraints for Neogene and Quaternary ignimbrites in the Central Andes (South Peru)

Science.gov (United States)

De La Rupelle, A.; Thouret, J. C.; Cubukcu, H. E.; Jicha, B.; Bréard, E.; Gerbe, M.-C.; Le Pennec, J.-L.; Diot, H.; Boivin, P.

2012-04-01

Central Andean deformation history in southern Peru is recorded in Neogene volcanic units of Ocoña and Cotahuasi canyons that cut across the western Cordillera. Acceleration (100 km3) Nazca (c.24.6 Ma), Alpabamba (19.4-18.0 Ma), and Huaylillas (14.25-12.7 Ma) ignimbrite sheets preceded the canyon incision, whereas sheets of smaller volume (Peru, stratigraphy, chronology, AMS, fabric, Neogene, Quaternary.

Dynamics of prolonged salt movement in the Glückstadt Graben (NW Germany) driven by tectonic and sedimentary processes

Science.gov (United States)

Warsitzka, Michael; Kley, Jonas; Jähne-Klingberg, Fabian; Kukowski, Nina

2017-01-01

The formation of salt structures exerted a major influence on the evolution of subsidence and sedimentation patterns in the Glückstadt Graben, which is part of the Central European Basin System and comprises a post-Permian sediment thickness of up to 11 km. Driven by regional tectonics and differential loading, large salt diapirs, salt walls and salt pillows developed. The resulting salt flow significantly influenced sediment distribution in the peripheral sinks adjacent to the salt structures and overprinted the regional subsidence patterns. In this study, we investigate the geometric and temporal evolution of salt structures and subsidence patterns in the central Glückstadt Graben. Along a key geological cross section, the post-Permian strata were sequentially decompacted and restored in order to reconstruct the subsidence history of minibasins between the salt structures. The structural restoration reveals that subsidence of peripheral sinks and salt structure growth were initiated in Early to Middle Triassic time. From the Late Triassic to the Middle Jurassic, salt movement and salt structure growth never ceased, but were faster during periods of crustal extension. Following a phase from Late Jurassic to the end of the early Late Cretaceous, in which minor salt flow occurred, salt movement was renewed, particularly in the marginal parts of the Glückstadt Graben. Subsidence rates and tectonic subsidence derived from backstripping of 1D profiles reveal that especially the Early Triassic and Middle Keuper times were periods of regional extension. Three specific types of salt structures and adjacent peripheral sinks could be identified: (1) Graben centre salt walls possessing deep secondary peripheral sinks on the sides facing away from the basin centre, (2) platform salt walls, whose main peripheral sinks switched multiple times from one side of the salt wall to the other, and (3) Graben edge pillows, which show only one peripheral sink facing the basin centre.

Cooling history of the Valles Caldera, New Mexico using ESR dating method

International Nuclear Information System (INIS)

Ogoh, K.; Toyoda, S.; Ikeda, S.; Ikeya, M.; Goff, F.

1993-01-01

ESR dating was made at the Valles caldera by using the Al center and Ti center in quartz grains separated from the layers of the Valles Rhyolite. Obtained ESR ages were much younger than those by other methods (fission track and 39 Ar- 40 Ar). A reported thermal event of about 10-40 ka ago might explain the difference between the above ages. (author)

Xenarthra (Mammalia) from a new late Neogene fossiliferous locality in Northwestern Argentina

Science.gov (United States)

Zurita, Alfredo E.; Camacho, María; Miño-Boilini, Angel R.; Candela, Adriana M.; Cuadrelli, Francisco; Krmpotic, Cecilia M.; Solís, Natalia

2017-12-01

Northwestern Argentina contains one of the most complete continental late Neogene (ca. 9-2.58 Ma) fossiliferous sequences in South America, especially in the current territories of the Catamarca, Tucumán and Jujuy provinces. More precisely in Jujuy Province several localities bearing mainly fossil mammals have been reported at the Quebrada de Humahuaca in the Uquía, Maimará and Tilcara formations, in which the clade Xenarthra (Mammalia) is well-represented. In this scenario, the fossiliferous potential of other localities of Jujuy Province are less known, especially in those areas located at the northwest end of Argentina, bordering Bolivia in the Northern Puna. A new late Neogene fossiliferous locality near Calahoyo (3639 m.a.s.l), Jujuy Province, is here reported. The materials, belonging to Xenarthra, were exhumed from the base of the Tafna Formation which was deposited in a sedimentary basin by alluvial and/or fluvial currents, undergoing transitions of various lacustrine episodes. The taxa include the Tardigrada Pyramiodontherium bergi (Megatheriidae) and the Cingulata Eosclerocalyptus sp. (Glyptodontidae) and Macrochorobates chapalmalensis (Dasypodidae). From a biostratigraphic viewpoint, this assemblage suggests a Late Miocene-Pliocene age for the base of the Tafna Formation, and partially contradicts the supposed Plio-Pleistocene age of this unit. Finally, the new specimens here described indicate that Xenarthra were taxonomically and ecologically diverse during the late Neogene in the northwest end of Argentina, since they are represented by at least three main lineages (sloths, glyptodontids and armadillos).

Characterization of malaria mortality in Valle del Cauca, 2005-2006 Caracterización de la mortalidad por malaria en el Valle del Cauca, 2005-2006

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Gloria Castro

2009-12-01

Full Text Available Introduction. Valle del Cauca is one of the states in Colombia that reports a high number of deaths due to malaria. Understanding the basis of malarial deaths is useful for assessing the efficacy of the health system and to identify areas where improvements are necessary to decrease malaria mortality.
Objective. Potential determinants of mortality in malaria cases are characterized in a demographic study centered in Valle del Cauca.
Materials and methods. A descriptive analysis was directed to 25 cases of malaria death occurring in Valle del Cauca during 2005 and 2006.
Results. The mean age was 31.3 years (range, 2 to 71 yr, 11 were women (1 pregnant, 11 were from the malaria-endemic port of Buenaventura, and 5 from other Pacific coastal states. After entering the health system facility, the standard malaria diagnostic, the thick smear, was not ordered for 7 cases at any time during the treatment period. In cases where a thick smear was taken at first contact, 11 had a positive and 5 had a negative initial report. Cerebral malaria (7/18 cases and renal failure (6/18 cases were the most frequent complications. During hospitalization, 13/18 cases developed other complications, mainly acute lung edema (8/18 cases and shock (5/18 cases.
Conclusions. Failures in primary health care of patients with malaria were recognized. This information has been used to implement actions aimed at improving initial care of malaria subjects in the health services of Valle del Cauca. The study recommends that other states in Colombia increase their efforts to decrease malaria mortality.Introducción. El Valle del Cauca es uno de los departamentos que mayor número de muertes por paludismo reporta en Colombia. El análisis de estas muertes permite una aproximación diagnóstica al funcionamiento del sistema de salud y contribuye a generar propuestas tendientes a disminuir la mortalidad por esta enfermedad.
Objetivo. Caracterizar demogr

Wrench tectonics control on Neogene-Quaternary sedimentation along the Mid-Hungarian Mobile Belt

Science.gov (United States)

Pogacsas, Gyorgy; Juhász, Györgyi; Mádl-Szőnyi, Judit; Simon, Szilvia; Lukács, Szilveszter; Csizmeg, János

2010-05-01

terrain, lying originally between the Central Alpine and Southern Alpine units, reached its recent position by some hundred kilometers strike slip movement, resulting in shifting of depocenters from the SW toward NE. The TISZA unit was characterised by clockwise motion, while counterclockwise rotation of the ALPACA is inferred in Late Oligocene-Miocene. Lower Miocene layers were deposited in depocenters whose subsidence was initiated by escape tectonics, NE-ward displacement of the ALCAPA terrane, and uplifting of the NW-SE oriented Neo-Vardar zone. The Neo-Vardar zone was represented by wide area of continental and alluvial depositional systems. 2. During the middle-late Badenian (15.5-13.6Ma), the ALCAPA collided with the European platform, and the eastward movement of the Tisza-Dacia became pronounced. Because of that the former right lateral motion along the Mid-Hungarian Mobile Belt ceased and a long period of left lateral strike slipe began. Earlier development of pull-apart basins, related to the extensive strike-slip faulting inside the ALCAPA, changed to the graben opening driven by the westward subduction and the eastward motion of the Tisza-Dacia. The middle-late Badenian period was characterised by sediments deposited in listric fault bounded half grabens, in crestal collapse grabens related to (flat-ramp) listric faults, in wide and/or narrow rift systems. Migration of volcanic activity and facies belts took place during relatively short period of times. Large displacements along listric faults have resulted in tilting of originally horizontal strata, and the formation of a regional unconformity between the middle Miocene and the upper Miocene sediments. Wrench fault related pull apart basins were filled by terrestrial to marine sediments. 3. During the Sarmatian-Pannonian (13.6-6.2 Ma), while the eastward motion of the ALPACA was strictly restricted, the Tisza-Dacia unit was able still to move eastward until the last parts of the remnant Carpathian Flysch

Stratigraphy of Neogene deposits in the Rethymnon Province, Crete, with special reference to the phylogeny of uniserial Uvigerina from the Mediterranean region

NARCIS (Netherlands)

Meulenkamp, J.E.

1969-01-01

Stratigraphical and micropaleontological investigations were performed on Neogene deposits of the Rethymnon Province, Western Crete. The Neogene succession includes marine as well as brackish and fresh-water sediments. Eight formations are recognized, several of which have to be regarded as

Decapod crustaceans from the Neogene of the Caribbean: diversity, distribution and prospectus

NARCIS (Netherlands)

Collins, J.S.H.; Portell, R.W.; Donovan, S.K.

2009-01-01

The Neogene decapod crustaceans are reviewed from Aruba, Bonaire and Curaçao, Anguilla, Barbados, Carriacou, Costa Rica, Cuba, Florida, Hispaniola (Haiti and Dominican Republic), Jamaica, Mexico, Panama, Puerto Rico, St. Kitts, Tintamare Island, Trinidad and Venezuela. The most widely distributed

The Late Neogene elephantoid-bearing faunas of Indonesia and their palaeozoogeographic implications

NARCIS (Netherlands)

Bergh, van den G.D.

1999-01-01

The stratigraphic framework of the Neogene fossil vertebrate bearing formations of the Indonesianislands Sulawesi and Flores is established and the sediments are dated by means of marinemicropalaeontological and/or palaeomagnetic methods. The results allow comparison of the faunaevolution on these

Deeply concealed half-graben at the SW margin of the East European Craton (SE Poland — Evidence for Neoproterozoic rifting prior to the break-up of Rodinia

Directory of Open Access Journals (Sweden)

P. Krzywiec

2018-01-01

Full Text Available Baltica was one of continents formed as a result of Rodinia break-up 850–550 Ma. It was separated from Amazonia(? by the Tornquist Ocean, the opening of which was preceded by Neoproterozoic extension in a network of continental rifts. Some of these rifts were subsequently aborted whereas the Tornquist Rift gave rise to splitting of Rodinia and formation of the Tornquist Ocean. The results of 1-D subsidence analysis at the fossil passive margin of Baltica provided insight in the timing and kinematics of continental rifting that led to break-up of Rodinia. Rifting was associated with Neoproterozoic syn-rift subsidence accompanied by deposition of continental coarse-grained sediments and emplacement of continental basalts. Transition from a syn-rift to post-rift phase in the latest Ediacaran to earliest early Cambrian was concomitant with deposition of continental conglomerates and arkoses, laterally passing into mudstones. An extensional scenario of the break-up of Rodinia along the Tornquist Rift is based on the character of tectonic subsidence curves, evolution of syn-rift and post-rift depocenters in time, as well as geochemistry and geochronology of the syn-rift volcanics. It is additionally reinforced by the high-quality deep seismic reflection data from SE Poland, located above the SW edge of the East European Craton. The seismic data allowed for identification of a deeply buried (11–18 km, well-preserved extensional half-graben, developed in the Palaeoproterozoic crystalline basement and filled with a Neoproterozoic syn-rift volcano-sedimentary succession. The results of depth-to-basement study based on integration of seismic and gravity data show the distribution of local NE–SW elongated Neoproterozoic depocenters within the SW slope of the East European Craton. Furthermore, they document the rapid south-eastwards thickness increase of the Neoproterozoic succession towards the NW–SE oriented craton margin. This provides evidence

Shed Some Light on the Subject: Teaching Ramon del Valle-Inclan's "Luces de bohemia"

Science.gov (United States)

Parker, Jason Thomas

2011-01-01

This essay seeks to provide parallel and interchangeable approaches to teaching Ramon del Valle-Inclan's challenging play "Luces de bohemia". A greater understanding of the cultural and mental frameworks of the early twentieth-century Spanish spectator will permit students to penetrate the dense intertextuality that characterizes Valle's…

Paleogeographic and Depositional Model for the Neogene fluvial succession, Pishin Belt Northwest Pakistan

DEFF Research Database (Denmark)

Kasi, Aimal Khan; Kassi, Akhtar Muhammad; Umar, Muhammad

2017-01-01

Miocene subaerial sedimentation started after the final closure of Katawaz Remnant Ocean. Based on detailed field data twelve facies were recognized in Neogene successions exposed in Pishin Belt. These facies were further organized into four facies associations i.e. channels, crevasse splay, natural levee...... and floodplain facies associations. Facies associations and variations provided ample evidences to recognize number of fluvial architectural components in the succession e.g., low-sinuosity sandy braided river, mixed-load meandering, high-sinuosity meandering channels, single-story sandstone and/or conglomerate...... channels, lateral accretion surfaces (point bars) and alluvial fans. Neogene sedimentation in the Pishin Belt was mainly controlled by active tectonism and thrusting in response to oblique collision of the Indian Plate with Afghan Block of the Eurasian Plate along the Chaman-Nushki Fault. Post Miocene...

Active tectonics of the southeastern Upper Rhine Graben, Freiburg area (Germany)

Science.gov (United States)

Nivière, B.; Bruestle, A.; Bertrand, G.; Carretier, S.; Behrmann, J.; Gourry, J.-C.

2008-03-01

The Upper Rhine Graben has two Plio-Quaternary depocentres usually interpreted as resulting from tectonic reactivation. The southern basin, near Freiburg im Breisgau (Germany), contains up to 250 m of sediments. Beneath the younger alluvial deposits related to the current drainage system, a former river network deeply entrenched in the substratum reveals a very low regional base level of early Pleistocene age. The offset of channels at faults allows us to infer a Pleistocene reactivation of the syn-rift fault pattern and the estimation of slip rates. Maximum vertical movements along the faults have not exceeded 0.1 mm/yr since the middle Pleistocene. Current activity is concentrated along the westernmost faults. Morphologic markers indicate late Pleistocene reactivation of the Rhine River fault, and geophysical prospecting suggests a near-surface offset of young sedimentary deposits. The size of the fault segments potentially reactivated suggests that earthquakes with magnitude larger than Mw=6.3 could be expected in the area with a return interval of about 8000 years. Extrapolated to the duration of the Plio-Pleistocene, the strain rate estimates reveal that the tectonic forcing may account for only one-third to one-half of the whole thickness of the Plio-Pleistocene sediments of the basin fill. Thus other processes must be invoked to understand the growth of the Plio-Pleistocene basin. Especially the piracy of the Rhine River to the north during the early Pleistocene could explain these effects.

Kadunud üheksakümnendad / Valle-Sten Maiste

Index Scriptorium Estoniae

Maiste, Valle-Sten, 1972-

1999-01-01

Sisaldab 2 proosaraamatute loetelu: 1998 a. ilmunud proosaraamatuid ; Eesti iseseisvusaastate proosa tipud ja täpid : [1992-1997]. Eesti kirjandusest 1990-ndatel. Vastukaja : Raudam, Toomas. Valle-Sten Maiste surm ja igavene elu // Sirp (1999) 16. apr., lk. 7

Tectono-volcanic control of fissure type vents for the 28 Ma Panalillo ignimbrite in the Villa de Reyes Graben, San Luis PotosI, Mexico

International Nuclear Information System (INIS)

Tristan-Gonzalez, Margarito; Labarthe-Hernandez, Guillermo; Aguillon-Robles, Alfredo; Aguirre-DIaz, Gerardo J

2008-01-01

The volcano-tectonic events at the Villa de Reyes Graben (VRG), in the southern Sierra Madre Occidental, Mexico, include 1) a regional NNE fault system developed before 32 Ma, 2) this pre-32 Ma faulting controlled the emplacement of 31.5 Ma dacitic domes, 3) NE faulting at 28 Ma that displaced the 31.5 Ma dacitic domes and formed the VRG, as well as the oblique grabens of Bledos and Enramadas oriented NW, 4) emplacement of Panalillo ignimbrite at 28 Ma filling the VRG and erupting from fissures related to the oblique grabens, and eruption of Placa basalt apparently also from fault-controlled vents.

Tectono-volcanic control of fissure type vents for the 28 Ma Panalillo ignimbrite in the Villa de Reyes Graben, San Luis PotosI, Mexico

Energy Technology Data Exchange (ETDEWEB)

Tristan-Gonzalez, Margarito; Labarthe-Hernandez, Guillermo; Aguillon-Robles, Alfredo [Instituto de Geologia/DES IngenierIa, UASLP, Av. Dr. Manuel Nava 5, Zona Universitaria, C.P. 78240, San Luis PotosI, S.L.P. (Mexico); Aguirre-DIaz, Gerardo J [Centro de Geociencias, Universidad Nacional Autonoma de Mexico, Campus Juriquilla, Queretaro, 76230 (Mexico)], E-mail: mtiistan@uasln.mx, E-mail: ger@geociencias.unam.mx

2008-10-01

The volcano-tectonic events at the Villa de Reyes Graben (VRG), in the southern Sierra Madre Occidental, Mexico, include 1) a regional NNE fault system developed before 32 Ma, 2) this pre-32 Ma faulting controlled the emplacement of 31.5 Ma dacitic domes, 3) NE faulting at 28 Ma that displaced the 31.5 Ma dacitic domes and formed the VRG, as well as the oblique grabens of Bledos and Enramadas oriented NW, 4) emplacement of Panalillo ignimbrite at 28 Ma filling the VRG and erupting from fissures related to the oblique grabens, and eruption of Placa basalt apparently also from fault-controlled vents.

Neogene sedimentation on the outer continental margin, southern Bering Sea

Science.gov (United States)

Vallier, T.L.; Underwood, M.B.; Gardner, J.V.; Barron, J.A.

1980-01-01

Neogene sedimentary rocks and sediments from sites on the outer continental margin in the southern Bering Sea and on the Alaska Peninsula are dominated by volcanic components that probably were eroded from an emergent Aleutian Ridge. A mainland continental source is subordinate. Most sediment in the marine environment was transported to the depositional sites by longshore currents, debris flows, and turbidity currents during times when sea level was near the outermost continental shelf. Fluctuations of sea level are ascribed both to worldwide glacio-eustatic effects and to regional vertical tectonics. Large drainage systems, such as the Yukon and Kuskokwim Rivers, had little direct influence on sedimentation along the continental slope and Unmak Plateau in the southern Bering Sea. Sediments from those drainage systems probably were transported to the floor of the Aleutian Basin, to the numerous shelf basins that underlie the outer continental shelf, and to the Arctic Ocean after passing through the Bering Strait. Environments of deposition at the sites along the outer continental margin have not changed significantly since the middle Miocene. The site on the Alaska Peninsula, however, is now emergent following shallow-marine and transitional sedimentation during the Neogene. ?? 1980.

Thermal maturity and petroleum kitchen areas of Liassic Black Shales (Lower Jurassic) in the central Upper Rhine Graben, Germany

Science.gov (United States)

Böcker, Johannes; Littke, Ralf

2016-03-01

In the central Upper Rhine Graben (URG), several major oil fields have been sourced by Liassic Black Shales. In particular, the Posidonia Shale (Lias ɛ, Lower Toarcian) acts as excellent and most prominent source rock in the central URG. This study is the first comprehensive synthesis of Liassic maturity data in the URG area and SW Germany. The thermal maturity of the Liassic Black Shales has been analysed by vitrinite reflectance (VRr) measurements, which have been verified with T max and spore coloration index (SCI) data. In outcrops and shallow wells (oil window (ca. 0.50-0.60 % VRr). This maturity is found in Liassic outcrops and shallow wells in the entire URG area and surrounding Swabian Jura Mountains. Maximum temperatures of the Posidonia Shale before graben formation are in the order of 80-90 °C. These values were likely reached during Late Cretaceous times due to significant Upper Jurassic and minor Cretaceous deposition and influenced by higher heat flows of the beginning rift event at about 70 Ma. In this regard, the consistent regional maturity data (VRr, T max, SCI) of 0.5-0.6 % VRr for the Posidonia Shale close to surface suggest a major burial-controlled maturation before graben formation. These consistent maturity data for Liassic outcrops and shallow wells imply no significant oil generation and expulsion from the Posidonia Shale before formation of the URG. A detailed VRr map has been created using VRr values of 31 wells and outcrops with a structure map of the Posidonia Shale as reference map for a depth-dependent gridding operation. Highest maturity levels occur in the area of the Rastatt Trough (ca. 1.5 % VRr) and along the graben axis with partly very high VRr gradients (e.g. well Scheibenhardt 2). In these deep graben areas, the maximum temperatures which were reached during upper Oligocene to Miocene times greatly exceed those during the Cretaceous.

El Camino de los Llanos - entre los valles de Chicama y Moche

OpenAIRE

Bernabé Romero, Joseph A.; Ministerio de Cultura

2014-01-01

Un indicador importante para la identificación del camino de la costa es su infraestructura lineal o la rectitud de su trazo, sobre todo al ingreso de los valles irrigados, siempre orientado de Norte – Sur, cruza la franja costera de forma longitudinal asociado a caminos trasversales que continúan por los principales valles. Otro aspecto a destacar del camino costero es su asociación a sitios locales que pueden o no tener componentes incas en su conformación.

Neogene sharks and rays from the Brazilian 'Blue Amazon'.

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Orangel Aguilera

Full Text Available The lower Miocene Pirabas Formation in the North of Brazil was deposited under influence of the proto-Amazon River and is characterized by large changes in the ecological niches from the early Miocene onwards. To evaluate these ecological changes, the elasmobranch fauna of the fully marine, carbonate-rich beds was investigated. A diverse fauna with 24 taxa of sharks and rays was identified with the dominant groups being carcharhiniforms and myliobatiforms. This faunal composition is similar to other early Miocene assemblages from the proto-Carribbean bioprovince. However, the Pirabas Formation has unique features compared to the other localities; being the only Neogene fossil fish assemblage described from the Atlantic coast of Tropical Americas. Phosphate oxygen isotope composition of elasmobranch teeth served as proxies for paleotemperatures and paleoecology. The data are compatible with a predominantly tropical marine setting with recognized inshore and offshore habitats with some probable depth preferences (e.g., Aetomylaeus groups. Paleohabitat of taxa particularly found in the Neogene of the Americas (†Carcharhinus ackermannii, †Aetomylaeus cubensis are estimated to have been principally coastal and shallow waters. Larger variation among the few analyzed modern selachians reflects a larger range for the isotopic composition of recent seawater compared to the early Miocene. This probably links to an increased influence of the Amazon River in the coastal regions during the Holocene.

Fault rocks and veins formation in the crystalline Palaeozoic basement of the N margin of the Littoral Chain (Catalan Coastal Ranges, NE Spain)

Science.gov (United States)

Alías, Gemma; Belmonte, Alba; Cantarero, Irene; Inglés, Montserrat; Travé, Anna

2013-04-01

The Littoral Chain corresponds to a horst of NE-SW direction formed during the Neogene extension which in the studied area (Collserola-Montnegre massif) is mainly composed by Paleozoic materials. At the northern margin the horst limits with the Vallès basin which is infilled by Miocene detrital materials. In the Forques Hill, two km to the est of Martorell, an excellent outcrop of Ordovician phyllites summarise an spread tectonic evolution from Hercynian to Neogene deformation. This work evaluates the behaviour of phyllites during the Hercynian ductile deformation and later during the fragile Mesozoic and Neogene tectonics. The weakness of these rocks together with the situation very close to the Vallès Fault favour that this area concentrates many deformation structures related to extensional tectonics, such as veins, cataclasites and gouges. Phyllites present a pervasive regional hercynian foliation oriented WNW-ESE and dipping moderately to the NNE; a huge amount of quartz veins, up to 20% of the rock volume, were injected during and immediately after the main foliation development. Two groups of fractures cutting the phyllites can be distinguished in the field according to the fault rock products, the vein infilling, the orientation and the geometry. The first one corresponds to Mesozoic fractures that have a NE-SW trend and dip indistinctly to the NW or SE, in a conjugate system. They are characterized by the formation of a broad zone of 0,2 m up to 1,5 m formed either by cataclasites or en echelon veins that indicate a normal movement. The cataclasites are cohesive greenish rocks, with 50% of clasts of wall rock from mm to dm in size. Neoformed minerals in the matrix are chlorite - albite - barite ± titanite and rutile. Veins are white to pinkish in colour and two types of infill have been identified: albite - chlorite - iron oxides± rutile and dolomite - chlorite. The second group belongs to Neogene fractures which although similar orientation than those

Gastropoda-Bivalvia Fauna And Neogene-Quaternary Stratigraphy of the Southwest of Dardanelles (Çanakkale-NWAnatolia)

Science.gov (United States)

Kapan, Sevinç; Kabasakal, Sinem

2016-04-01

Gastropoda-Bivalvia Fauna And Neogene-Quaternary Stratigraphy of the Southwest of Dardanelles (Çanakkale-NWAnatolia) Sevinç KAPAN, Sinem KABASAKAL, Çanakkale Onsekiz Mart University, Engineering Faculty, Geological Engineering Department sevinckapan_yesilyurt@hotmail.com In this study, paleontology and stratigraphy of Neogene and Quaternary units around south of the Dardanelles have been examined using Gastropoda and Bivalvia fauna. In the investigation area, the base of the sediments that belongs to Neogene, consist of the volcanics which are formed with basalts, andesites and tuff. Neogene begins unconformity with basal conglomerate which are formed with basalt and tuff gravels. The measurable thickness of the Neogene sediments is approximately 200meters in total. First fossiliferius level which consist of Lymnocardium (Euxinicardium) nobile Sabba has showed similarities with the Pontian (Late Miocene) fauna of the Eastern Paratethys. The existence of Melanopsis and Psidium species indicate that the basin has been brackish water feeding by fresh water in the Early Pliocene. Theodoxus fluviatilis (Linne), Theodoxus (Calvertia) aff. imbricata Brusina, Theodoxus (Calvertia) licherdopoli scriptus (Stefanescu), Viviparus mammatus (Stefanescu), Valvata (Valavata) sulekiana Brusina, Valvata (Cincinna) crusitensis Fontannes, Hydrobia cf grandis Cobalcescu, Hydrobia ventrosa Monfort, Melanopsis (Melanopsis) cf. bergeroni Stefanescu, , Melanopsis (Melanopsis) sandbergeri rumana Tournouer, Melanopsis (Canthidomus) hybostoma anili Taner, Melanopsis (Canthidomus) hybostoma amaradica Fontannes, Melanopsis (Canthidomus) lanceolata Neumayr, Amphimelania fossariformis (Tournouer), Melanoides tuberculata monolithica (Bukowski), Radix (Radix) peregra (Müller), Planorbarius thiollierei (Michaud), Potamida (Potamida) craiovensis craiovensis (Tournouer), Potamida (Potamida) berbestiensis (Fontannes), Unio pristinus davilai Porumbaru, Unio subexquisitus Jatzko, Anadonta zmaji

Changes of the fluid regime behaviour through time in fault zones (Catalan Coastal Ranges, NE Spain)

Science.gov (United States)

Cantarero, Irene; Lanari, Pierre; Alías, Gemma; Travé, Anna; Vidal, Olivier; Baqués, Vinyet

2013-04-01

Most Neogene normal faults of the central Catalan Coastal Ranges are the reactivation of previous normal Mesozoic faults and Paleogene thrust faults. These faults, such as the Vallès and the Hospital faults, are characterised by developing polyphasic fault-fluid systems. These systems have been inferred from regional to thin section scale observations combined with geochemical analyses. Moreover, the neoformation of chlorite and K-white mica in fault rocks has allowed us to constrain the P-T conditions during fault evolution using thermodynamic modelling. In these two faults, deformation is mainly localized in the basement granodiorite from the footwall. As a whole, four tectonic events have been distinguished. The first event corresponds to the Hercynian compression, which is characterised by mylonite bands in the Hospital fault. After this first compressional event and during the exhumation of the pluton, crystallization of M1 and M2 muscovite and microcline occurred in the Vallès fault as result of deuteric alteration, at temperatures between 330°C and 370°C. The second event, attributed to the Mesozoic rifting, is characterized by precipitation of M3 and M4 phengite together with chlorite and calcite C1 at temperatures between 190 and 310°C. These minerals precipitated from a fluid resulting from the mixing between marine waters and meteoric waters, which had been warmed at depth, upflowing along the faults. The third event, corresponding to the Paleogene compression, is characterised by low-temperature meteoric fluids, responsible of precipitation of calcite C2, in the Hospital fault. In the Vallès fault, the Paleogene compression generated a shortcut that produced a blue gouge and the uplift of the Mesozoic structures, avoiding the formation of new minerals within them. Finally, the fourth event, related to the Neogene extension, was responsible of syn-rift cements such as chlorite, calcite C4 and laumontite in the Vallès fault and calcite C3 in the

Peligros hidrometeorológicos en un valle árido: abordaje geopedológico

Directory of Open Access Journals (Sweden)

Raúl Emmanuel Ocaña

2018-01-01

Full Text Available Se expone el análisis geopedológico del valle intermontano de Zonda, Argentina, con el objetivo de que este sea aplicado en estudios de ordenamiento territorial. Los resultados indican que los riesgos provienen de tres cuencas principales: dos locales (bajadas pedemontanas, río Seco de la Ciénaga y una regional (río San Juan, cada una con sus propias características. Los peligros más importantes corresponden a procesos de aluviones e inundaciones provenientes de los límites del valle y desbordes de los máximos caudales estivales del río San Juan. Los resultados fueron presentados en mapas que contienen unidades de relieve y riesgos hidrometeorológicos asociados. Los asentamientos humanos crecen en el valle en contacto con el piedemonte y están amenazados principalmente por aluviones de recurrencia anual y estival.

Peligros hidrometeorológicos en un valle árido: abordaje geopedológico

Directory of Open Access Journals (Sweden)

Raúl Emmanuel Ocaña

2018-01-01

Full Text Available Se expone el análisis geopedológico del valle intermontano de Zonda, Argentina, con el objetivo de que este sea aplicado en estudios de ordenamiento territorial. Los resultados indican que los riesgos provienen de tres cuencas principales: dos locales (río San Juan, río Seco de la Ciénaga y una regional (bajadas pedemontanas, cada una con sus propias características. Los peligros más importantes corresponden a procesos de aluviones e inundaciones provenientes de los límites del valle y desbordes de los máximos caudales estivales del río San Juan. Los resultados fueron presentados en mapas que contienen unidades de relieve y riesgos hidrometeorológicos asociados. Los asentamientos humanos crecen en el valle en contacto con el piedemonte y están amenazados principalmente por aluviones de recurrencia anual y estival.

Neogene displacements in the Solomon Islands Arc

Science.gov (United States)

Ridgway, J.

1987-02-01

The geology and present configuration of the Solomon Island arc can be explained in terms of the Neogene displacement of a single linear chain of islands. The central part of an original arc consisting of Bougainville, Choiseul, Santa Ysabel, Guadalcanal and San Cristobal was displaced to the northeast as a consequence of the attempted subduction of the Woodlark spreading system. Malaita arose on the northeastern side of the arc as a result of interaction between the arc and the Pacific Ocean floor and the volcanic islands of the New Georgia group formed to the southwest in response to the subduction of a spreading ridge, thus giving rise to the present double chain structure of the arc.

Polimorfismos de grupos sanguíneos en Cachi, Valle Calchaqui, Salta

OpenAIRE

Acreche, Noemí; Albeza, María V.; Caruso, Graciela; Acosta, Rebeca; Felix, Sebastián

2001-01-01

El Departamento de Cachi, en la Provincia de Salta pertenece a los Valles Calchaquíes, los que se extienden además por Catamarca y Tucumán, constituyéndose en una región importante en la comunicación entre el Valle de Lerma y la Puna. Hasta el momento no se conocen datos de la genética de estas poblaciones, salvo los publicados por Matson en 1968 registrados en otra región de la provincia. A partir de la determinación de los grupos: ABO, MN, Ss, Cc, Dd, Ee, P, Diego y Kell-Cellano, Duffy y...

Lembah Elqui / Valle de Elqui / Elqui Valley

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Ian Campbell

2017-05-01

Full Text Available The three versions of Ian Campbell’s poem about Valle de Elqui (in Chile presented here comprise a poem he first wrote in Spanish, then in English and finally in a more powerful version in Indonesian, which was published in 2012 in the literary pages of the Jakarta mass media daily Kompas. Campbell regards this whole process as emblematic of his explorations in trilingual poetics, namely what does a ‘concept’/poem idea look like if done in the three languages with which he has some degree of written knowledge or fluency: English, Spanish, Indonesian. This mirrors the ‘three-pronged’ title ‘Selatan-Sur-South’ that he adopted for the collection of his poetry in PORTAL vol. 5, no. 1, 2008. The Indonesian version, ‘Lembah Elqui, ‘was included in Campbell’s poetry and prose collection Tak ada Peringatan (Vivid Publishing, 2013. In each version now the reference is to Gabriela Mistral (1889-1957, Nobel Prize Laureate for Literature (1945, whose burial place lies in Monte Grande in the Valle de Elqui in northern Chile.

Geothermal hydrology of Valles Caldera and the southwestern Jemez Mountains, New Mexico

Science.gov (United States)

Trainer, Frank W.; Rogers, Robert J.; Sorey, M.L.

2000-01-01

The Jemez Mountains in north-central New Mexico are volcanic in origin and have a large central caldera known as Valles Caldera. The mountains contain the Valles geothermal system, which was investigated during 1970-82 as a source of geothermal energy. This report describes the geothermal hydrology of the Jemez Mountains and presents results of an earlier 1972-75 U.S. Geological Survey study of the area in light of more recent information. Several distinct types of thermal and nonthermal ground water are recognized in the Jemez Mountains. Two types of near-surface thermal water are in the caldera: thermal meteoric water and acid sulfate water. The principal reservoir of geothermal fluids is at depth under the central and western parts of the caldera. Nonthermal ground water in Valles Caldera occurs in diverse perched aquifers and deeper valley-fill aquifers. The geothermal reservoir is recharged by meteorically derived water that moves downward from the aquifers in the caldera fill to depths of 6,500 feet or more and at temperatures reaching about 330 degrees Celsius. The heated geothermal water rises convectively to depths of 2,000 feet or less and mixes with other ground water as it flows away from the geothermal reservoir. A vapor zone containing steam, carbon dioxide, and other gases exists above parts of the liquid-dominated geothermal zone. Two subsystems are generally recognized within the larger geothermal system: the Redondo Creek subsystem and the Sulphur Creek subsystem. The permeability in the Redondo Creek subsystem is controlled by stratigraphy and fault-related structures. Most of the permeability is in the high-angle, normal faults and associated fractures that form the Redondo Creek Graben. Faults and related fractures control the flow of thermal fluids in the subsystem, which is bounded by high-angle faults. The Redondo Creek subsystem has been more extensively studied than other parts of the system. The Sulphur Springs subsystem is not as well

New evidence of cenozoic tectonism in the southeastern region of Brazil: the Barra de Sao Joao graben in Cabo Frio platform

International Nuclear Information System (INIS)

Mohriak, W.U.

1990-01-01

The western portion of the Campos Basin is limited by a hinge line that limits the deposition of pre-Aptian sediments in the offshore region. The Cabo Frio arch corresponds to a platform with smaller relative subsidence, where Tertiary sediments are deposited directly on shallow basement rocks. A conspicuous asymmetric graben occurs in the offshore region between Buzios and Macae. This rhomb-graben measures 20 km by 40 km, with the longer axis trending NE. The geological and geophysical characteristics of the Barra de Sao Joao graben supports a genetic affiliation with the onshore Taubate, Resende and Volta Redonda basins, rather than with the Campos Basin. The latter basin was formed in the Neocomian by rupturing of the Pangea, while the radiometric age determination of ankaramitic lavas near Volta Redonda suggests that the onshore basins were formed during the Eocene or Early Oligocene. A better understanding of the crustal geometry and the postulation of geodynamic models for these sedimentary basins will result from the integration of the onshore geology with the subsurface data presented in this paper. (author)

Bioethics and Climate Change: A Response to Macpherson and Valles.

Science.gov (United States)

Resnik, David B

2016-10-01

Two articles published in Bioethics recently have explored the ways that bioethics can contribute to the climate change debate. Cheryl Cox Macpherson argues that bioethicists can play an important role in the climate change debate by helping the public to better understand the values at stake and the trade-offs that must be made in individual and social choices, and Sean Valles claims that bioethicists can contribute to the debate by framing the issues in terms of the public health impacts of climate change. While Macpherson and Valles make valid points concerning a potential role for bioethics in the climate change debate, it is important to recognize that much more than ethical analysis and reflection will be needed to significantly impact public attitudes and government policies. © 2016 John Wiley & Sons Ltd.

Neogene sharks and rays from the Brazilian ‘Blue Amazon’

Science.gov (United States)

Aguilera, Orangel; Carrillo-Briceño, Jorge D.; Kocsis, László; Vennemann, Torsten W.; de Toledo, Peter Mann; Nogueira, Afonso; Amorim, Kamilla Borges; Moraes-Santos, Heloísa; Polck, Marcia Reis; Ruivo, Maria de Lourdes; Linhares, Ana Paula; Monteiro-Neto, Cassiano

2017-01-01

The lower Miocene Pirabas Formation in the North of Brazil was deposited under influence of the proto-Amazon River and is characterized by large changes in the ecological niches from the early Miocene onwards. To evaluate these ecological changes, the elasmobranch fauna of the fully marine, carbonate-rich beds was investigated. A diverse fauna with 24 taxa of sharks and rays was identified with the dominant groups being carcharhiniforms and myliobatiforms. This faunal composition is similar to other early Miocene assemblages from the proto-Carribbean bioprovince. However, the Pirabas Formation has unique features compared to the other localities; being the only Neogene fossil fish assemblage described from the Atlantic coast of Tropical Americas. Phosphate oxygen isotope composition of elasmobranch teeth served as proxies for paleotemperatures and paleoecology. The data are compatible with a predominantly tropical marine setting with recognized inshore and offshore habitats with some probable depth preferences (e.g., Aetomylaeus groups). Paleohabitat of taxa particularly found in the Neogene of the Americas (†Carcharhinus ackermannii, †Aetomylaeus cubensis) are estimated to have been principally coastal and shallow waters. Larger variation among the few analyzed modern selachians reflects a larger range for the isotopic composition of recent seawater compared to the early Miocene. This probably links to an increased influence of the Amazon River in the coastal regions during the Holocene. PMID:28832664

Characterization of Pliocene and Miocene Formations in the Wilmington Graben, Offshore Los Angeles, for Large-Scale Geologic Storage of CO₂

Energy Technology Data Exchange (ETDEWEB)

Bruno, Michael [Geomechanics Technologies, Incorporated, Monrovia, CA (United States)

2014-12-08

Geomechanics Technologies has completed a detailed characterization study of the Wilmington Graben offshore Southern California area for large-scale CO₂ storage. This effort has included: an evaluation of existing wells in both State and Federal waters, field acquisition of about 175 km (109 mi) of new seismic data, new well drilling, development of integrated 3D geologic, geomechanics, and fluid flow models for the area. The geologic analysis indicates that more than 796 MMt of storage capacity is available within the Pliocene and Miocene formations in the Graben for midrange geologic estimates (P50). Geomechanical analyses indicate that injection can be conducted without significant risk for surface deformation, induced stresses or fault activation. Numerical analysis of fluid migration indicates that injection into the Pliocene Formation at depths of 1525 m (5000 ft) would lead to undesirable vertical migration of the CO₂ plume. Recent well drilling however, indicates that deeper sand is present at depths exceeding 2135 m (7000 ft), which could be viable for large volume storage. For vertical containment, injection would need to be limited to about 250,000 metric tons per year per well, would need to be placed at depths greater than 7000ft, and would need to be placed in new wells located at least 1 mile from any existing offset wells. As a practical matter, this would likely limit storage operations in the Wilmington Graben to about 1 million tons per year or less. A quantitative risk analysis for the Wilmington Graben indicate that such large scale CO₂ storage in the area would represent higher risk than other similar size projects in the US and overseas.

Nesting ecology of the olive ridley sea turtle (Lepidochelys olivacea) (Cheloniidae) at el Valle Beach, northern pacific, Colombia; Ecologia de anidacion de la tortuga golfina (Lepidochelys olivacea) (Cheloniidae) en la Playa El Valle, pacifico norte, Colombia

Energy Technology Data Exchange (ETDEWEB)

Barrientos Munoz, Karla G; Gallego, Cristian Ramirez; Paez, Vivian

2014-07-01

The olive ridley (Lepidochelys olivacea) is the most common sea turtle to nest in Colombia. El valle beach is considered the most important nesting beach for this species in South America. Intensive direct capture of nesting females and egg poaching for consumption and local commercial purposes has been a common practice for years. We conducted an analysis of the nesting ecology of the olive ridley on el valle beach in the northern pacific of Colombia in 2008. A total of 164 clutches were transferred to an artificial hatchery for protection. The peak of nesting occurred from the second half of August until the end of September, accounting for 64.6 % of all nests. Along the beach, the section most frequently used was section 3, with 26 % of the nests. The nests were laid mainly in zone 3.69 %. We encountered 55 nesting females and marked 46 of them. Mean CCL was 64.9 ± 2.4 cm and mean CCW was 68.6 ± 2.6 cm. females laid on average of 87.3 ± 14.2 eggs per clutch. We recorded two nesting events per female, with a mean inter-nesting period of 18.8 ± 4.2 days. The reproductive output for the season was 181.5 ± 34.8 eggs / female. Mean hatching success was 81.1 ± 12.1 % and mean emergence success was 77.6 ± 12.7 %. The incubation period was 65 ± 4.7 days. Our study is a valuable contribution to knowledge of the reproductive ecology of the olive ridley population regionally and globally.

The Geometry of the Aquifer's System of the Terraguelt Graben by the Gravimetry and the Electric Prospecting

International Nuclear Information System (INIS)

Brahmia, A.; Hani, A.; Lamouroux, C.

2009-01-01

The goal of the present survey is the determination of the shape of Terraguelt graben aquifer system. The gravimetric survey brings a satisfactory answer in this sense that the residual anomaly map made appear a negative anomaly of - 20 m Gals and that the gradient delimits the Graben enough well. The electric survey on the basis of the geologic information and the few mechanical boring achieved in the plain permits to retail the facies of the replenishment better. Indeed some either the length of the current electrode AB line, the center of the plain makes appear of weak values of apparent resistivity, the shalky limestone substratum of age superior Maestrichien is not reached in spite of a length of AB line = 3000 m. Whereas the borders appear with resistivities more important, in the center of the plain these last become more and more weak with the increase of the AB length. The shape of the Graben is illustrated well in the electric cross sections and is confirmed by the interrelationship of the lithostratigraphique columns of the mechanical boring. The interpretation of mechanical boring data shows two principals aquifers : the first one is included in the karstified limestone of upper Maestrichien and the second one is in the replenishment constituted by sand, and gravel, pebble. This replenishment is estimated at 1200 m thickness. The piezo metric maps shows that the aquifers are feeded from the the East and South mountains borders

Sedimentary evidence of historical and prehistorical earthquakes along the Venta de Bravo Fault System, Acambay Graben (Central Mexico)

Science.gov (United States)

Lacan, Pierre; Ortuño, María; Audin, Laurence; Perea, Hector; Baize, Stephane; Aguirre-Díaz, Gerardo; Zúñiga, F. Ramón

2018-03-01

The Venta de Bravo normal fault is one of the longest structures in the intra-arc fault system of the Trans-Mexican Volcanic Belt. It defines, together with the Pastores Fault, the 80 km long southern margin of the Acambay Graben. We focus on the westernmost segment of the Venta de Bravo Fault and provide new paleoseismological information, evaluate its earthquake history, and assess the related seismic hazard. We analyzed five trenches, distributed at three different sites, in which Holocene surface faulting offsets interbedded volcanoclastic, fluvio-lacustrine and colluvial deposits. Despite the lack of known historical destructive earthquakes along this fault, we found evidence of at least eight earthquakes during the late Quaternary. Our results indicate that this is one of the major seismic sources of the Acambay Graben, capable of producing by itself earthquakes with magnitudes (MW) up to 6.9, with a slip rate of 0.22-0.24 mm yr- 1 and a recurrence interval between 1940 and 2390 years. In addition, a possible multi-fault rupture of the Venta de Bravo Fault together with other faults of the Acambay Graben could result in a MW > 7 earthquake. These new slip rates, earthquake recurrence rates, and estimation of slips per event help advance our understanding of the seismic hazard posed by the Venta de Bravo Fault and provide new parameters for further hazard assessment.

Zeolites of the Valle Central of Costa Rica and its outskirts; Zeolitas del Valle Central de Costa Rica y sus alrededores

Energy Technology Data Exchange (ETDEWEB)

Zeledon, Luis Alonso [Moravia, San Jose, (Costa Rica)

2004-12-15

19 different species of zeolites have been found in 25 outcrops in the Valle Central of Costa Rica and in the Siquirres region. All the zeolites are secondary minerals and crystallized in little veins and vesicles of the basalts and pyroclastics rocks of the La Cruz and Grifo Alto formations, belonging to the Aguacate Group and the alkaline igneous rocks of Guayacan. The most frequent species of zeolites are stibnite, chabasite, laumontite, mesolite/mordenite, thomsonite, and analcime. Natrolite only was found near to Siquirres. (Author) [Spanish] Se describen 19 especies diferentes de zeolitas procedentes de 25 afloramientos en los alrededores del Valle Central de Costa Rica y en la region de Siquirres. Todas las zeolitas descritas son de origen secundario y se presentan en vetillas y vesiculas de los basaltos y rocas piroclasticas de las formaciones La Cruz y Grifo Alto del Grupo Aguacate y en las rocas igneas alcalinas de Guayacan. Las especies mas frecuentes son estilbita, chabasita, laumontita, mesolita/modernita, thomsonita y analcima. La natrolita solo se encontro en los alrededores de Siquirres. (Autor)

Tectonic Evolution of the Çayirhan Neogene Basin (Ankara), Central Turkey

Science.gov (United States)

Behzad, Bezhan; Koral, Hayrettin; İşb&idot; l, Duygu; Karaaǧa; ç, Serdal

2016-04-01

Çayırhan (Ankara) is located at crossroads of the Western Anatolian extensional region, analogous to the Basin and Range Province, and suture zone of the Neotethys-Ocean, which is locus of the North Anatolian Transform since the Late Miocene. To the north of Çayırhan (Ankara), a Neogene sedimentary basin comprises Lower-Middle Miocene and Upper Miocene age formations, characterized by swamp, fluvial and lacustrine settings respectively. This sequence is folded and transected by neotectonic faults. The Sekli thrust fault is older than the Lower-Middle Miocene age formations. The Davutoǧlan fault is younger than the Lower-Middle Miocene formations and is contemporaneous to the Upper Miocene formation. The Çatalkaya fault is younger than the Upper Miocene formation. The sedimentary and tectonic features provide information on mode, timing and evolution of this Neogene age sedimentary basin in Central Turkey. It is concluded that the region underwent a period of uplift and erosion under the influence of contractional tectonics prior to the Early-Middle Miocene, before becoming a semi-closed basin under influence of transtensional tectonics during the Early-Middle Miocene and under influence of predominantly extensional tectonics during the post-Late Miocene times. Keywords: Tectonics, Extension, Transtension, Stratigraphy, Neotectonic features.

Rifting in heterogeneous lithosphere inferences from numerical modeling of the northern North Sea and the Oslo Graben.

NARCIS (Netherlands)

Pascal Candas, C.; Cloetingh, S.A.P.L.

2002-01-01

Permian rifting and magmatism are widely documented across NW Europe. The different Permian basins often display contrasting structural styles and evolved in lithospheric domains with contrasting past evolution and contrasting thermotectonic ages. In particular, the Oslo Graben and the northern

Stratigraphy of the layered terrain in Valles Marineris, Mars

Science.gov (United States)

Komatsu, G.; Strom, Roger G.

1991-01-01

The layered terrain in Valles Marineris provides information about its origin and the geologic history of this canyon system. Whether the terrain is sedimentary material deposited in a dry or lacustrine environment, or volcanic material related to the tectonics of the canyon is still controversial. However, recent studies of Gangis Layered Terrain suggests a cyclic sequence of deposition and erosion under episodic lacustrine conditions. The stratigraphic studies are extended to four other occurrences of layered terrains in Valles Marineris in an attempt to correlate and distinguish between depositional environments. The Juvantae Chasma, Hebes Chasma, Ophir and Candor Chasmata, Melas Chasma, and Gangis Layered Terrain were examined. Although there are broad similarities among the layered terrains, no two deposits are exactly alike. This suggests that there was no synchronized regional depositional processes to form all the layered deposits. However, the similar erosional style of the lower massive weakly bedded unit in Hebes, Gangis, and Ophir-Candor suggests it may have been deposited under similar circumstances.

niñez en el valle del cauca (Colombia

Directory of Open Access Journals (Sweden)

Luis Fernando Aguado Quintero

2007-01-01

Full Text Available Se construye un Indicador de Carencias en la Niñez (icn para los 42 municipios que integran el departamento del Valle del Cauca. El índice agrupa un conjunto de indicadores en áreas sensibles al bienestar de la población menor de 15 años de edad: asistencia escolar, cobertura de aseguramiento en la atención de servicios de salud y déficit cualitativo de la vivienda. Los principales resultados muestran que la brecha de carencias infantiles más grande la presenta el municipio de Buenaventura, con un icn de 0.40 y la menor la reporta el municipio de Cali (0.17. Igualmente, con respecto al acceso a servicios sociales básicos para los niños, se hace evidente la gran distancia entre la capital y el promedio departamental, y entre éste último y los municipios más rezagados que conforman la subregión norte del departamento del Valle del Cauca.

Extensional tectonics and sedimentary response of the Early–Middle Cambrian passive continental margin, Tarim Basin, Northwest China

Directory of Open Access Journals (Sweden)

Zhiqian Gao

2012-09-01

Full Text Available The fact that several half-grabens and normal faults developed in the Lower–Middle Cambrian of Tazhong (central Tarim Basin and Bachu areas in Tarim Basin, northwest China, indicates that Tarim Basin was under extensional tectonic setting at this time. The half-grabens occur within a linear zone and the normal faults are arranged in en echelon patterns with gradually increasing displacement eastward. Extensional tectonics resulted in the formation of a passive continental margin in the southwest and a cratonic margin depression in the east, and most importantly, influenced the development of a three-pronged rift in the northeast margin of the Tarim Basin. The fault system controlled the development of platform – slope – bathyal facies sedimentation of mainly limestone-dolomite-gypsum rock-saline rock-red beds in the half-grabens. The NW-SE trending half-grabens reflect the distribution of buried basement faults.

Intrapopulational genic variation of the giant African Snail (Achatina fulica in the Valle del Cauca

Directory of Open Access Journals (Sweden)

Angie Patiño-Montoya

2017-05-01

Full Text Available Objective. To evaluate the intrapopulation genetic variation of A. fulica in the Valle del Cauca. Materials and methods. Ten microsatellite loci from specimens collected at eight municipalities in the Valle del Cauca Department were amplified. Allelic frequencies and descriptors of intrapopulation genetic diversity were estimated. Bayesian analysis was used to estimate the number of groups present in the study area. Results. Two groups were identified in the Valle del Cauca (p > 50%: one group comprised individuals from the north and center of the department, and one group comprised individuals from the south and west of the department. These groups were genetically different from each other (FST 0.16; p<0.05. Isolation by distance was confirmed (Mantel p 0.01; R2 0.06, and a high level of endogamy was detected through a deficit of heterozygotes in the evaluated loci (FIS 0.45. Conclusions. We suggest that the A. fulica population present in the Valle del Cauca could have been introduced at more than one location, or that there could have been more than one wave of invasion. The high level of endogamy is probably the result of control activities that eliminated adult individuals in the population, which has led to an enhanced founder effect.

High-resolution sedimentological and subsidence analysis of the Late Neogene, Pannonian Basin, Hungary

Science.gov (United States)

Juhasz, E.; Muller, P.; Toth-Makk, A.; Hamor, T.; Farkas-Bulla, J.; Suto-Szentai, M.; Phillips, R.L.; Ricketts, B.

1996-01-01

Detailed sedimentological and paleontological analyses were carried out on more than 13,000 m of core from ten boreholes in the Late Neogene sediments of the Pannonian Basin, Hungary. These data provide the basis for determining the character of high-order depositional cycles and their stacking patterns. In the Late Neogene sediments of the Pannonian Basin there are two third-order sequences: the Late Miocene and the Pliocene ones. The Miocene sequence shows a regressive, upward-coarsening trend. There are four distinguishable sedimentary units in this sequence: the basal transgressive, the lower aggradational, the progradational and the upper aggradational units. The Pliocene sequence is also of aggradational character. The progradation does not coincide in time in the wells within the basin. The character of the relative water-level curves is similar throughout the basin but shows only very faint similarity to the sea-level curve. Therefore, it is unlikely that eustasy played any significant role in the pattern of basin filling. Rather, the dominant controls were the rapidly changing basin subsidence and high sedimentation rates, together with possible climatic factors.

Reassessment of 50 years of seismicity in Simav-Gediz grabens (Western Turkey), based on earthquake relocations

Science.gov (United States)

Karasozen, E.; Nissen, E.; Bergman, E. A.; Walters, R. J.

2013-12-01

Western Turkey is a rapidly deforming region with a long history of high-magnitude normal faulting earthquakes. However, the locations and slip rates of the responsible faults are poorly constrained. Here, we reassess a series of large instrumental earthquakes in the Simav-Gediz region, an area exhibiting a strong E-W gradient in N-S extension rates, from low rates bordering the Anatolian Plateau to much higher rates in the west. We start with investigating a recent Mw 5.9 earthquake at Simav (19 May 2011) using InSAR, teleseismic body-wave modeling and field observations. Next, we exploit the small but clear InSAR signal to relocate a series of older, larger earthquakes, using a calibrated earthquake relocation method which is based on the hypocentroidial decomposition (HDC) method for multiple event relocation. These improved locations in turn provide an opportunity to reassess the regional style of deformation. One interesting aspect of these earthquakes is that the largest (the Mw 7.2 Gediz earthquake, March 1970) occurred in an area of slow extension and indistinct surface faulting, whilst the well-defined and more rapidly extending Simav graben has ruptured in several smaller, Mw 6 events. However, our relocations highlight the existence of a significant gap in instrumental earthquakes along the central Simav graben, which, if it ruptured in a single event, could equal ~Mw 7. We were unable to identify fault scarps along this section due to dense vegetation and human modification, and we suggest that acquiring LiDAR data in this area should be a high priority in order to properly investigate earthquake hazard in the Simav graben.

Mineral inclusions in placer zircon from the Ohře (Eger) Graben: New data on „strontiopyrochlore“

Czech Academy of Sciences Publication Activity Database

Seifert, W.; Förster, H.-J.; Rhede, D.; Tietz, O.; Ulrych, Jaromír

2012-01-01

Roč. 92, 1/2 (2012), s. 39-53 ISSN 0930-0708 R&D Projects: GA ČR(CZ) GA205/09/1170 Institutional support: RVO:67985831 Keywords : Eger Graben * zircon * "strontiopyrochlore" Subject RIV: DB - Geology ; Mineralogy Impact factor: 1.681, year: 2012

Kinematic models of extensional structures

International Nuclear Information System (INIS)

Groshong, R.H. Jr.

1990-01-01

This paper discusses kinematic models that can relate faults of different types and different positions within a single dynamic system and thereby offer the potential to explain the disparate seismic activity characteristic of extensional terrains. The major styles are full grabens, half grabens, domino blocks, and glide-block systems. Half grabens, the most likely models for Basin and Range structure, are formed above a master fault of decreasing dip with depth and a hangingwall that deforms as it passes over the curved fault. Second-order normal faults, typically domino style, accommodate the required hangingwall deformation. According to the author low-angle detachment faults are consistent with the evidence of seismicity only on high-angle faults if the hangingwall of the detachment is broken by multiple half-graben systems

Vaya valle: "Aquellas escuelas olvidadas"

Directory of Open Access Journals (Sweden)

Consuelo Olea Cuena

2010-12-01

Full Text Available (ES El "CEIP Virgen de la Velilla" es una escuela situada en la zona Sur de Cantabria, en el municipio de Valderredible. En ella, hemos desarrollado "Vaya valle: Aquellas Escuelas Olvidadas" que se trata de un proyecto anual en el que todas las personas de la escuela, cada una a su nivel, investigan para saber qué ha sucedido con las antiguas escuelas que tenemos desperdigadas por los pueblos. En tiempos de nuestros abuelos y padres, había una o dos escuelas en la mayor parte de los 52 pueblos del valle. De manera que hemos ido de escuela en escuela para escuchar y tomar nota de cómo era el día a día en todas esas escuelas. Ello siempre a través de diferentes relatos en boca de nuestros padres, de nuestros abuelos, o de otras personas que nos hemos encontrado en los pueblos. El alumnado pudo observar cómo eran los edificios, comprobó cual es su estado actual y la función que desempeñan hoy día. Hemos respirado el polvo de los materiales que nos íbamos encontrando, jugando a los juegos que jugaban entonces, escuchando algunas historias tradicionales, e imaginando las situaciones anecdóticas que nos narraban. Con un final más o menos triste, esas escuelas han ido haciéndose más y más pequeñas, hasta llegar a olvidarse tras las concentraciones escolares. Mediante este artículo explicativo, nos gustaría compartir con vosotros nuestra experiencia a nivel pedagógico y organizativo.

Reactivation of mass movements in Dessie graben, the example of an active landslide area in the Ethiopian Highlands

Czech Academy of Sciences Publication Activity Database

Vařilová, Z.; Kropáček, J.; Zvelebil, J.; Šťastný, Martin; Vilímek, V.

2015-01-01

Roč. 12, č. 5 (2015), s. 985-996 ISSN 1612-510X Institutional support: RVO:67985831 Keywords : Dessie graben * Ethiopian highlands * human impact * landslides * natural hazards Subject RIV: DB - Geology ; Mineralogy Impact factor: 3.049, year: 2015

[Renal biopsy practice in Piedmont and Valle d'Aosta].

Science.gov (United States)

Manganaro, Marco; Nebiolo, Pier Eugenio; Rollino, Cristiana; Giacchino, Franca; Savoldi, Silvana; Besso, Luca; Colla, Loredana; Amore, Alessandro; Ferro, Michela; Marazzi, Federico; Chiarinotti, Doriana; Guarnieri, Andrea; Quaglia, Marco; Manes, Massimo; Vaccaro, Valentina; Marcuccio, Cristina; Licata, Carolina; Patti, Rosaria; Mariano, Filippo; Bongi, Anna Maria; Biamino, Ercole; Boschetti, Maria Antonietta; Della Volpe, Mario; Malcangi, Ugo; Baroni, Adriana; Vagelli, Giuseppe; Costantini, Luigia; Salomone, Mario; Formica, Marco; Caramello, Elisa; Campo, Andrea; Pignone, Eugenia; Messuerotti, Alessandra; Roccatello, Dario; Stratta, Piero; Segoloni, Giuseppe; Coppo, Rosanna

2012-01-01

In 2010 a questionnaire was administered to the renal units of Piedmont and Valle d'Aosta to analyze their procedures for renal biopsy (RB). Seventy-eight percent of units performed RBs, 57% for more than 20 years, but only 43% performed at least 20 BRs per year. 20/21 units performed RB in an inpatient setting and 1/21 in day hospital with the patient remaining under observation the night after. Thirty-two percent did not consider a single kidney as a contraindication to RB, 59% considered it a relative contraindication and 9% considered it an absolute contraindication. In 90.5% of units there was a specific protocol for patient preparation for RB and 86% used a specific informed consent form. Ninety-five percent of units performed ultrasound-guided RB, 60% of them using needle guides attached to the probe. In 81% of units the left side was preferred; 71% put a pillow under the patient's abdomen. All units used disposable, automated or semi-automated needles. Needle size was 16G in 29%, 18G in 58%, and both 16G and 18G in 14% of units; 1 to 3 samples were drawn. One third of units had a microscope available for immediate evaluation of specimen adequacy. After RB, 86% of units kept patients in the prone position for 2-6 hours and all prescribed a period of bed rest (at least 24 hours in 90.5%). 90.5% of units followed a specific postbiopsy observation protocol consisting of blood pressure, heart rate and red blood cell measurements at different times, and urine monitoring and ultrasound control within 12-24 hours (only half of them also employing color Doppler). One third of all units discharged patients after 1 day and two thirds after 2-3 days; all prescribed abstention from effort and from antiplatelet drugs for 7-15 days. In 9 units both RB and tissue processing and examination were done in the same hospital, while 12 units sent the samples elsewhere. 76% obtained results in 2-4 days, 19% in 6-7 days, and 5% in 10-15 days. Less than 20% of the interviewed

Evaluación de los programas de control prenatal para adolescentes en el valle de Aburrá, 2003 Evaluation of prenatal control programs offered to teenagers in Valle de Aburrá, Colombia, 2003

OpenAIRE

Carlos Adolfo Salazar; Margarita María Ortiz Mesa; María Isabel Martínez Ortiz; Andrea González Morales; Joaquín Guillermo Gómez Dávila

2004-01-01

Objetivo: la investigación que se presenta a continuación tuvo como objetivo identificar y evaluar los programas de control prenatal para adolescentes ofrecidos en el valle de Aburrá, Antioquia, Colombia, durante el año 2003. Materiales y métodos: se revisaron varias fuentes primarias y se elaboró un listado de todas las instituciones de salud del valle de Aburrá. Se hicieron entrevistas telefónicas con los respectivos directores para establecer cuáles instituciones tenían un programa de cont...

Estimating regional pore pressure distribution using 3D seismic velocities in the Dutch Central North Sea Graben

NARCIS (Netherlands)

Winthaegen, P.L.A.; Verweij, J.M.

2003-01-01

The application of the empirical Eaton method to calibrated sonic well information and 3D seismic interval velocity data in the southeastern part of the Central North Sea Graben, using the Japsen (Glob. Planet. Change 24 (2000) 189) normal velocitydepth trend, resulted in the identification of an

En reise i tid og landskap – Planlegging og tilrettelegging i kulturlandskapet, Valle i Setesdal

OpenAIRE

Hillestad, Ingunn

2010-01-01

Oppgaven omhandler hvordan fremtidig utvikling i Valle i Setesdal kan legges tilrette gjennom lansdskapsplanlegging. Selve initiativet kom fra Valle kommune, men jeg har stått fritt i forhold til vinklingen av oppgaven. Målet er å aktivisere Nomeland, et sentrumsnært område og omkringliggende steder. Planleggingen skal rettes mot friluftsliv og kultur. Et annet mål er å få en bred og sammensatt brukergruppe, med forankring i lokalbefolkningen og et tilbud for turister. Oppgaven er strukturert...

Estudio hidrogeológico del valle de Mala

OpenAIRE

Ministerio de Agricultura. Dirección General de Aguas, Suelos e Irrigaciones

1980-01-01

Determina el recurso hídrico subterráneo del valle del río Mala, mediante el análisis e investigación de las características hidrogeológicas, en base a las informaciones de diferentes etapas del estudio; para de esta manera, racionalizar mejor su uso, dando cumplimiento así a lo dispuesto por la Ley General de Aguas.

Popkultuurgi on rahvuskultuuri osa / Valle-Sten Maiste ja Jan Kaus

Index Scriptorium Estoniae

Maiste, Valle-Sten, 1972-

2009-01-01

Õnnestunud muusikafestival Tallinn Music Week tõstatas olulisi kultuuripoliitilisi küsimusi. Jan Kaus ja Valle-Sten Maiste arutlevad artiklis selle üle, et popkultuur vajaks hariduse ja tugistruktuuride näol toestamist, tuleks tunnustada kodumaist väärt pop- ja rockmuusikat

Neogene stratigraphy and Andean geodynamics of southern Ecuador

Science.gov (United States)

Hungerbühler, Dominik; Steinmann, Michael; Winkler, Wilfried; Seward, Diane; Egüez, Arturo; Peterson, Dawn E.; Helg, Urs; Hammer, Cliff

2002-01-01

The present paper reviews Tertiary volcanic and sedimentary formations in the Inter-Andean region of southern Ecuador (between 2°S and 4°20'S) in order to develop a geodynamic model of the region. The formations occur in the southern shallow prolongation of the Inter-Andean Valley between the Cordillera Real to the east, and the Cordillera Occidental and Amotape-Tahuín Provinces to the west. One hundred fifty zircon fission-track analyses has established a detailed chronostratigraphy for the sedimentary and volcanic formations and several small intrusions. The Paleogene to early Miocene formations are dominated by intermediate and acidic volcanic and pyroclastic rocks. In addition, relics of Eocene continental sedimentary series have been identified. The Neogene sedimentary series lie unconformably on deformed and eroded metamorphic, sedimentary and volcanic formations. They were deposited in two stages, which are separated by a major unconformity dated at ≈10-9 Ma. (1) During the middle and early late Miocene (≈15-10 Ma) marginal marine deltaic, lagoonal, lacustrine and fluvial environments prevailed, which we group under the heading "Pacific Coastal sequences". They presumably covered a greater surface area in southern Ecuador than their present occurrence in small topographic depressions. We suggest that they were deposited in the shallow marine Cuenca and Loja Embayments. Deposition in a marginal marine environment is also supported by the occurrence of brackish water ostracods and other fauna. (2) Above the regional (angular) unconformity, the coastal facies are overlain by late Miocene (≈9-5 Ma) continental alluvial fan and fluvial facies which are in turn covered by mainly airborne volcanic material. They represent the "Intermontane sequences" of the basins of Cuenca, Girón-Santa Isabel, Nabón, Loja and Malacatos-Vilcabamba. Sedimentologic and stratigraphic results are used to discuss the tectonic setting of Neogene sedimentation in the forearc

Stratigraphy, sedimentology and petrology of neogene rocks in the Deschutes Basin, Central Oregon: a record of continental-margin volcanism and its influence on fluvial sedimentation in an arc-adjacent basin

International Nuclear Information System (INIS)

Smith, G.A.

1986-07-01

Neogene rocks of the Deschutes basin include the middle Miocene Columbia River Basalt Group and Simtustus Formation, and late Miocene to early Pliocene Deschutes Formation. Assignment of Prineville chemical-type flows to the Grande Ronde Basalt of the Columbia River Basalt Group is based on correlation of these lavas from their type area through the Deschutes basin and onto the Columbia Plateau, where they have been previously mapped as Grande Ronde Basalt. Simtustus Formation is a newly defined unit intercalated with and conformable upon these basalts, and is unconformably overlain by Deschutes Formation. Burial of mature topography by middle Miocene basalts raised local base levels and initiated aggradation by low-gradient streams within the basin represented by the tuffaceous sandstones and mudstones of the Simtustus Formation. These sediments are enriched in pyroclastic constituents relative to contemporaneous Western Cascades volcanics, reflecting preferential incorporation of easily eroded and more widespread pyroclastic debris in distal sedimentary sequences compared to epiclastic contributions from lavas. The abundance of basalts, combined with the paucity of hydrous minerals and FeO and TiO 2 enrichment in intermediate lavas, characterizes early High Cascade volcanics as atypical for convergent-margin arcs. These petrologic characteristics are consistent with high-level fractionation in an extensional regime. Extension culminated in the development of an intra-arc graben, which ended Deschutes Formation deposition by structurally isolating the basin from the High Cascade source area

Identidades en movimiento: familias chilenas en la fruticultura del Alto Valle de Río Negro, Argentina Identities in movement: chilean families in the fruit production of the Alto Valle de Río Negro, Argentina

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Verónica Trpin

2007-12-01

Full Text Available Este artículo, basado en el trabajo de campo realizado en áreas rurales del Alto Valle de Río Negro, Argentina, desde el año 1999, tiene como propósito presentar las relaciones en las cuales se insertan hombres y mujeres chilenas que residen y trabajan en "chacras" destinadas a la producción frutícola. Las diferentes actividades en las chacras se organizan según el sexo y la edad, definiéndose una segmentación del mercado de trabajo en la que se ven involucrados los diferentes miembros de la familia. Como desarrollaré, ser trabajadores chilenos en la fruticultura del Alto Valle de Río Negro reproduce una identidad étnica y nacional en el seno de la cotidianeidad familiar y laboral.This article, based on field work conducted in rural areas of the Alto Valle de Río Negro, Argentina, from 1999 on, analyzes the relations in which Chilean men and women who reside and work in small farms destined to fruit production are inserted. The different activities in the small farms are organized according to sex and age, circumscribing a segment of the labor market in which different members of the family are involved. As I will demonstrate, to be a Chilean worker in the fruit growing region of the Alto Valle is to reproduce an ethnic and national identity through work routines mediated by family relations.

Caracterización del sector cooperativo de ahorro y crédito en el Valle del Cauca

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Ximena Sánchez Mayorga

2008-01-01

Full Text Available El artículo presenta una caracterización del sector cooperativo de ahorro y crédito en el Valle del Cauca, el cual es uno de los objetivos a desarrollar en el proyecto de investigación "Análisis del sector cooperativo de ahorro y crédito en el Valle del Cauca y propuesta de estrategia. Caso Cooperativa de Ahorro del Valle", del Grupo de Investigación Gestión y Productividad Contable. El estudio muestra la dinámica de crecimiento que ha tenido el sector cooperativo de ahorro y crédito en el Valle del Cauca en los últimos cinco años, aportando a la bancarización en Colombia; también se revisa el sector de economía solidaria en Colombia, presentando estadísticas que permiten visualizar lo que representa este sector en la economía del país. Se identifican en el Valle del Cauca las entidades dedicadas a la actividad de ahorro y crédito, planteándose las diferencias entre estas entidades y los establecimientos bancarios del sector financiero tradicional, resaltando el aporte de las cooperativas de ahorro y crédito a la estrategia del Gobierno Nacional definida como la banca de oportunidades1; puesto que en estas entidades hay igualdad social para sus asociados, logrando que un mayor número de personas accedan a los servicios financieros, aportando al desarrollo económico de las localidades donde funcionan.

CONSIDERACIONES SOBRE LAS ALGAS DEL VALLE DE TEHUACÁN-CUICATLÁN

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Eberto Novelo

2012-01-01

Full Text Available El Valle de Tehuacán-Cuicatlán es una zona semiárida que presenta una flora de algas rica en los cuerpos de agua temporales y permanentes, consta de 357 especies, muchas de ellas no registradas previamente en México: 183 especies de Bacillariophyta representan cerca del 50 % de la flora; 81 especies de Cyanoprokaryota constituyen el 22 % de la misma, 77 especies de Chlorophyta aportan el 20 % de la riqueza; complementan la flora 10 especies de Euglenophyta (2.8 %, 5 especies de Heterokontophyta (1.4 % y una especie de Rhodophyta (0.2 %. Las especies más frecuentes y más ampliamente distribuidas son en su mayoría alcalífilas y eurihalobias. Sin embargo, la mayoría de las especies se distribuyen principalmente en una o dos localidades y en dos tipos de ambientes (canales de riego y charcos. Se discute sobre la heterogeneidad de la composición tomando en cuenta la frecuencia de aparición en las muestras y en las cuatro zonas del Valle y el significado de esa distribución. El análisis de distribución y dominancia de las especies sugiere que las condiciones acuáticas del Valle son muy cambiantes y ello promueve la proliferación de especies de un espectro ecológico amplio, dentro de los límites generales de alcalinidad y salinidad moderadas.

Herencia materna en poblaciones de Puna y Valle Calchaqui - Salta

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Albeza, María V.

2005-01-01

Full Text Available Las poblaciones de la Puna y el Valle Calchaquí han sido estudiadas, tanto desde la perspectiva demográfica como de marcadores genéticos clásicos y nucleares. En este trabajo se analizan las secuencias de la región hipervariable I del mtDNA, en muestras de 100 individuos de diferentes localidades. La zona comprendida entre las posiciones 15997-16400 según la secuencia Anderson (región hipervariable I-HVRI fue secuenciada. El motivo RFLP- 7025 AluI fue adicionalmente analizado en las muestras para determinar su inclusión dentro del haplogrupo H. Las muestras que resultaron no-H fueron asignadas a distintos haplogrupos. Se han detectado un total de 34 haplotipos distintos definidos por 50 posiciones variables de los que una muy baja proporción (13,1 % resultaron haplotipos únicos. Sólo 4 de los 34 haplotipos son compartidos entre la población de la Puna y la de los Valles.

Comparative mortality patterns among the black population and the white-mestizo in Cali and Valle

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Fernando Urrea-Giraldo

2015-08-01

Full Text Available The article analyzes the patterns of comparative mortality of Cali and Valle, between the Afrodescendant and white-mestizo population, by sex and age groups, based on the metadata of deaths in the 2005 Census and the death certificate of the year 2010. The findings reveal strong differentials by age structures of deaths (pyramids and the cumulative mortality, which are conclusive of unequal mortality patterns between the two populations, both in Cali and Valle. This evinces demography of social inequality based on ethnic-racial component.

DIAGNÓSTICO Y PROPUESTA PARA UNA GESTIÓN INTEGRAL DEL RIESGO EN EL VALLE DE ABURRA: RED RIESGOS

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ARISTIZÁBAL EDIER

2010-05-01

Full Text Available A partir del análisis de la situación organizacional de las diferentes instituciones en el Valle de Aburrá frente a la reducción de desastres y emergencias asociadas con los fenómenos de origen natural y antrópico, el Área Metropolitana del Valle de Aburrá, como autoridad ambiental y entidad planificadora, hace una propuesta que pretende articular todas las entidades, organizaciones e instituciones públicas y privadas hacia una gestión integral del riesgo, y la cual denominó: Red para la Gestión del Riesgo en el Valle de Aburrá, Red Riesgos. Red Riesgos es un sistema organizacional abierto de carácter interinstitucional para orientar y coordinar las políticas y acciones de análisis y reducción de riesgos, preparación y ejecución de la respuesta y recuperación en casos de desastre y emergencias en el Valle de Aburrá. Como instrumento estratégico de la Red, se formuló el Plan Regional para la Gestión del Riesgo en el Valle de Aburrá que contiene las acciones que se deben ejecutar para la reducción de desastres y el manejo óptimo de los mismos y se diseñó el Sistema Integrado de Información para dar soporte a los diferentes procesos de gestión de la Red.

Nesting ecology of the olive ridley sea turtle (Lepidochelys olivacea) (Cheloniidae) at el Valle Beach, northern pacific, Colombia

International Nuclear Information System (INIS)

Karla G Barrientos Munoz; Cristian Ramirez Gallego; Vivian Paez

2014-01-01

The olive ridley (Lepidochelys olivacea) is the most common sea turtle to nest in Colombia. El valle beach is considered the most important nesting beach for this species in South America. Intensive direct capture of nesting females and egg poaching for consumption and local commercial purposes has been a common practice for years. We conducted an analysis of the nesting ecology of the olive ridley on el valle beach in the northern pacific of Colombia in 2008. A total of 164 clutches were transferred to an artificial hatchery for protection. The peak of nesting occurred from the second half of August until the end of September, accounting for 64.6 % of all nests. Along the beach, the section most frequently used was section 3, with 26 % of the nests. The nests were laid mainly in zone 3.69 %. We encountered 55 nesting females and marked 46 of them. Mean CCL was 64.9 ± 2.4 cm and mean CCW was 68.6 ± 2.6 cm. females laid on average of 87.3 ± 14.2 eggs per clutch. We recorded two nesting events per female, with a mean inter-nesting period of 18.8 ± 4.2 days. The reproductive output for the season was 181.5 ± 34.8 eggs / female. Mean hatching success was 81.1 ± 12.1 % and mean emergence success was 77.6 ± 12.7 %. The incubation period was 65 ± 4.7 days. Our study is a valuable contribution to knowledge of the reproductive ecology of the olive ridley population regionally and globally.

Major events in Neogene oxygen isotopic records

International Nuclear Information System (INIS)

Kennett, J.P.; Hodell, D.A.

1986-01-01

Changes in oxygen isotopic ratios of foraminiferal calcite during the cainozoic have been one of the primary tools for investigating the history of Arctic and Antarctic glaciation, although interpretations of the oxygen isotopic record differ markedly. The ambiguity in interpretation results mainly from the partitioning of temperature from ice volume effects in delta 18 O changes. Oxygen isotopic records for the Cainozoic show an increase in delta 18 O values towards the present, reflecting gradual cooling and increased glaciation of the Earth's climate since the late Cretaceous. A variety of core material from the South Atlantic and South-west Pacific oceans are investigated. This composite data represents one of the most complete available with which to evaluate the evolution of glaciation during the Neogene. Expansion of ice shelves in Antarctica undoubtedly accompanied the increased glaciation of the northern hemisphere, since eustatic sea-level lowering would positively reinforce ice growth on Antarctica

Caldera processes and magma-hydrothermal systems continental scientific drilling program: thermal regimes, Valles caldera research, scientific and management plan

Energy Technology Data Exchange (ETDEWEB)

Goff, F.; Nielson, D.L. (eds.)

1986-05-01

Long-range core-drilling operations and initial scientific investigations are described for four sites in the Valles caldera, New Mexico. The plan concentrates on the period 1986 to 1993 and has six primary objectives: (1) study the origin, evolution, physical/chemical dynamics of the vapor-dominated portion of the Valles geothermal system; (2) investigate the characteristics of caldera fill and mechanisms of caldera collapse and resurgence; (3) determine the physical/chemical conditions in the heat transfer zone between crystallizing plutons and the hydrothermal system; (4) study the mechanism of ore deposition in the caldera environment; (5) develop and test high-temperature drilling techniques and logging tools; and (6) evaluate the geothermal resource within a large silicic caldera. Core holes VC-2a (500 m) and VC-2b (2000 m) are planned in the Sulphur Springs area; these core holes will probe the vapor-dominated zone, the underlying hot-water-dominated zone, the boiling interface and probable ore deposition between the two zones, and the deep structure and stratigraphy along the western part of the Valles caldera fracture zone and resurgent dome. Core hole VC-3 will involve reopening existing well Baca number12 and deepening it from 3.2 km (present total depth) to 5.5 km, this core hole will penetrate the deep-crystallized silicic pluton, investigate conductive heat transfer in that zone, and study the evolution of the central resurgent dome. Core hole VC-4 is designed to penetrate deep into the presumably thick caldera fill in eastern Valles caldera and examine the relationship between caldera formation, sedimentation, tectonics, and volcanism. Core hole VC-5 is to test structure, stratigraphy, and magmatic evolution of pre-Valles caldera rocks, their relations to Valles caldera, and the influences of regional structure on volcanism and caldera formation.

Link between Neogene and modern sedimentary environments in the Zagros foreland basin

Science.gov (United States)

Pirouz, Mortaza; Simpson, Guy; Bahroudi, Abbas

2010-05-01

The Zagros mountain belt, with a length of 1800 km, is located in the south of Iran and was produced by collision between the Arabian plate and the Iran micro plate some time in the early Tertiary. After collision, the Zagros carbonate-dominated sedimentary basin has been replaced by a largely clastic system. The Neogene Zagros foreland basin comprises four main depositional environments which reflect the progressive southward migration of the deformation front with time. The oldest unit - the Gachsaran formation - is clastic in the northern part of the basin, but is dominated by evaporates in southern part, being deposited in a supratidal Sabkha-type environment. Overlying the Gachsaran is the Mishan formation, which is characterized by the Guri limestone member at the base, overlain by marine green marls. The thickness of the Guri member increases dramatically towards the southeast. The next youngest unit is the Aghajari Formation which consists of well sorted lenticular sandstone bodies in a red silty-mudstone. This formation is interpreted as representing the floodplain of dominantly meandering rivers. Finally, the Bakhtiari formation consists of mainly coarse-grained gravel sheets which are interpreted to represent braided river deposits. Each of these Neogene depositional environments has a modern day equivalent. For example, the braided rivers presently active in the Zagros mountains are modern analogues of the Bakhtiari. In the downstream direction, these braided rivers become meandering systems, which are equivalents of the Aghajari. Eventually, the meandering rivers meet the Persian gulf which is the site of the ‘modern day' Mishan shallow marine marls. Finally, the modern carbonate system on the southern margin of Persian Gulf represents the Guri member paleo-environment, behind which Sabkha-type deposits similar to the Gachsaran are presently being deposited. One important implication of this link between the Neogene foreland basin deposits and the

Expedition 354 on the Bengal fan: a Neogene record of Himalayan erosion

Science.gov (United States)

France-Lanord, C.; Spiess, V.; Schwenk, T.; Klaus, A.; Galy, A.

2017-12-01

Drilling in the Bengal fan generated a comprehensive record of Himalayan erosion over the Neogene and Quaternary. It documents the interplay between Himalayan tectonic and the monsoon. The fan is predominantly composed of detrital turbiditic sediments originating from Himalayan rivers, and transported through the delta and shelf canyon, supplying turbidity currents loaded with a wide spectrum of grain sizes. Turbiditic deposition makes that record at a given site is discontinuous which was the reason for an E-W transect approach. Exp. 354 drilled seven sites along a 320 km E-W transect at 8°N allowing the restitution of an almost complete record of Himalayan erosion at the scale of the Neogene. In spite of the transect's extension, a long absence of deposition was observed between 0.6 to 1.2 Ma indicating that turbiditic depocenter was derived more to the West for ca. 600 kyr. Turbidites have clear Himalayan origin with close mineralogical and isotopic analogy with those of the modern Ganga-Brahmaputra river sediments. Geochemistry shows relatively stable compositions throughout the Neogene and Quaternary and reveal a very weak regime of chemical weathering with no significant variation through time. Concentrations in mobile elements such as Na and K relative to Al are significantly higher than in modern sediments suggesting that weathering is amplified in the modern time. Low weathering of the sediments at 8°N indicates that erosion was dominated by physical processes and that transport is rapid enough to prevent evolution of particles in the floodplain. In the modern Himalaya, low weathering is achieved primarily by landslides and rapid transfer through the floodplain, i.e. limited recycling of sediment deposited in the floodplain. Both processes are favoured by the seasonality and the intensity of the monsoon. Although relatively stable, source tracers such as Sr-Nd isotopic compositions, and detrital carbonate compositions show organised variations with time

PALYNOLOGICAL MODEL OF THE LATE NEOGENE SEDIMENTS OF EASTERN SLAVONIA (CROATIA

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Gabrijela Pecimotika

2015-12-01

Full Text Available By applying a palynological analysis of the Late Neogene sediments from one exploration well in the area of Eastern Slavonia, three vegetation zones (Z1, Z2, Z3 as conditioned by climate sensitivity were set. On the basis of mutual percentage relations of the occurrence of individual form-species and grouping them according to the results of cluster analysis, these zones reflect the changes of warm-cold and variable humidity periods. The age of zones has been determined: zone Z1 is Pontian, zone Z2 is Pliocene and zone Z3 is Pleistocene-Holocene. In the Pontian, 13 form-species of spores were determined that do not cross the Miocene/Pliocene boundary. In the Pliocene, 4 index form-species of spores were determined that were not found in the Quaternary in the study area. In the youngest sediments of the study area, i.e. Pleistocene and Holocene, 7 index form-species of spores were determined. Together with well logging (gamma ray and specific resistivity logs of the formation, a model was constructed for the local routine provision of age in the study area. The results are generally consistent with other results obtained from Early Neogene sediments in adjacent areas in the central part of Paratethys, and may serve as a model for the correlation of contemporaneous sediments in other areas of Croatia, e.g. Sava and Drava Depressions , which in effect may contribute to the more efficient investigation of potential hydrocarbon reservoirs.

The Regional Water Cycle and Water Ice Clouds in the Tharsis - Valles Marineris System

Science.gov (United States)

Leung, C. W. S.; Rafkin, S. C.

2017-12-01

The regional atmospheric circulation on Mars is highly influenced by local topographic gradients. Terrain-following air parcels forced along the slopes of the major Tharsis volcanoes and the steep canyon walls of Valles Marineris significantly impact the local water vapor concentration and the associated conditions for cloud formation. Using a non-hydrostatic mesoscale atmospheric model with aerosol & cloud microphysics, we investigate the meteorological conditions for water ice cloud formation in the coupled Tharsis - Valles Marineris system near the aphelion season. The usage of a limited area regional model ensures that topographic slopes are well resolved compared to the typical resolutions of a global-coverage general circulation model. The effects of shadowing and slope angle geometries on the energy budget is also taken into account. Diurnal slope winds in complex terrains are typically characterized by the reversal of wind direction twice per sol: upslope during the day, and downslope at night. However, our simulation results of the regional circulation and diurnal water cycle indicate substantial asymmetries in the day-night circulation. The convergence of moist air masses enters Valles Marineris via easterly flows, whereas dry air sweep across the plateau of the canyon system from the south towards the north. We emphasize the non-uniform vertical distribution of water vapor in our model results. Water vapor mixing ratios in the lower planetary boundary layer may be factors greater than the mixing ratio aloft. Water ice clouds are important contributors to the climatic forcing on Mars, and their effects on the mesoscale circulations in the Tharsis - Valles Marineris region significantly contribute to the regional perturbations in the large-scale global atmospheric circulation.

Geomorphic response of an active metamorphic core-complex in a collisional orogen: Example from the Lunggar Shan, Southern Tibet

International Nuclear Information System (INIS)

Taylor, M H; Stockli, D F; Kapp, P A

2008-01-01

We present structural and neotectonic mapping from the Lunggar Shan rift in southern Tibet. The Lunggar Shan is a N-trending mountain range ∼70 km long N-S and up to 40 km wide E-W. The Lunggar Shan is bounded on its east side by a low-angle ( 0 ) east-dipping detachment fault that juxtaposes mylonitic gneiss and variably deformed granites in its footwall against alluvial fans and Neogene gravels in its hangingwall. Foliations in the mylonitic footwall dip 40 m of throw on individual scarps. An intriguing observation is that an intrabasinal topographic high is actively developing near areas of inferred maximum extension, with lacustrine sediments being uplifted and eroded. This observation indicates that the rift basin initially developed as a typical half-graben system that underwent a transition from deposition, to uplift and erosion perhaps as a result of isostatic rebound of the footwall at depth, warping the overlying hangingwall basin. If correct, the Lunggar Shan may represent a modern analogue to the supradetachment basin model

Qualité de l’air et nuisances sonores dans les vallées alpines de transit

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Jürg Thudium

2009-03-01

Full Text Available Les conséquences du trafic routier, en termes de nuisances sonores et de qualité de l’air, ont été analysées et comparées pour quatre vallées de transit alpin (Fréjus, Mont Blanc, Gothard et Brenner durant l’année 2004. Au regard du trafic alpin dans son ensemble, des disparités considérables apparaissent entre les vallées étudiées, mais également à l’intérieur de ces mêmes vallées. Les immissions (concentration de polluants produites par unité d’émission du trafic routier sont deux à trois fois plus élevées dans ces vallées alpines qu’en plaine. Ceci s’explique principalement par la topographie et le climat particuliers de ces vallées. À de nombreux points d’observation, les seuils d’immission ont été dépassés. Les vallées sont également affectées durement par la pollution sonore. « L’effet amphithéâtre » transporte le bruit à des altitudes supérieures, qui n’auraient pas été exposées à autant d’irradiation acoustique si la source de nuisances était située à égale distance, mais dans un « paysage ouvert ». De plus, la protection contre le bruit qui se réfléchit sur les pentes est malaisée. En résumé, toutes les vallées de transit étudiées peuvent être considérées comme des régions sensibles.The environmental consequences of road transport with regard to air and noise in the transit valleys of Fréjus, Mont-Blanc, Gotthard, and Brenner have been analysed and compared with each other for the year 2004. In respect of the share of transport passing through the Alps in transport as a whole, there are in part considerable differences between the valleys under investigation as well as within the individual valleys. The air pollution produced per emission unit of road transport is two to three times higher than in the open country, mainly because of the topography and the climate. At numerous monitoring points, the thresholds for the air pollution were exceeded

Disponibilidades hídricas para la forestación en el Valle de Calamuchita, Córdoba

OpenAIRE

Ravelo, Andrés Carlos; Zanvettor, R. E.; Ingaramo, P.

1997-01-01

p.111-116 Las disponibilidades hídricas para la forestación con Pinus elliottii y Pinus taeda en el valle de Calamuchita fueron analizadas utilizando el balance hídrico del suelo. Las similitudes de variables derivadas del balance hidrico para localidades del valle y localidades de origen de ambas especies indica condiciones adecuadas para el desarrollo de dichas especies. Mediante un análisis numérico de agregación se identifican a localidades del lugar de origen como posibles fuentes pro...

Depositional record of an avulsive fluvial system controlled by peat compaction (Neogene, Most Basin, Czech Republic)

Czech Academy of Sciences Publication Activity Database

Rajchl, M.; Uličný, David

2005-01-01

Roč. 52, č. 3 (2005), s. 601-625 ISSN 0037-0746 R&D Projects: GA ČR GA205/01/0629 Institutional research plan: CEZ:AV0Z30120515 Keywords : avulsion * Eger Graben * fluvial channels Subject RIV: DB - Geology ; Mineralogy Impact factor: 1.876, year: 2005

Micromammals (Insectivora; Rodentia of "Valle dell'Inferno" (Rome / Micromammiferi (Insectivora; Rodentia della Valle dell'Inferno (Roma

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Roberto Federici

1986-12-01

Full Text Available Abstract A research on micromammals in the area of "Valle dell'Inferno" (in the north-west of Rome was carried out. The study was based on a previous phytosociological survey which describes a Quercus suber population in the valley (a once larger residua1 of a roman cork-tree wood which is now included in the town. Specimens from Rodents (Apodemus sylvaticus, Mus domesticus, Rattus rattus, R. norvegicus, Pitymys savii and Insectivores (Crocidura suaveolens, Erinaceus europaeus were captured by live traps. Most of Insectivores specimens are represented by C. suaveolens. Generally C. suaveolens lives in sympatry with C. leucodon but no specimens of the latter were found in this area. Three different kinds of landscape are present in the "Inferno" valley, namely, the wood, the meadow, and the bottom valley (with high anthropic impact; we have compared these three landscapes with biotic indexes (index of faunistic affinity, index of biocoenotic affinity and index of environmental evaluation. We have also compared through the same indexes, the micromammal fauna of the "Inferno" valley with six other differently polluted localities in Latium, where animals were captured with the same live traps. This area retains its natura1 environment in despite of the high anthropic impact. Riassunto È stato effettuato uno studio sulla micromammalofauna terrestre della Valle dell'Inferno situata a nord-ovest di Roma. Lo studio è basato su una precedente indagine fitosociologica effettuata per la caratterizzazione vegetazionale di una sughereta un tempo molto estesa ed ora racchiusa nell'abitato cittadino. È stato pertanto possibile tracciare, tramite gli indici biotici, una correlazione tra microteriocenosi ed effetti dell'impatto antropico.

Estudio hidrogeológico del valle de Mala: nivel semidetallado

OpenAIRE

Ministerio de Agricultura y Alimentación. Dirección General de Aguas y Suelos; Proyecto Ampliación de la Frontera Agrícola con Utilización de Aguas Subterráneas

1980-01-01

Realiza la evaluación del potencial acuífero subterráneo disponible y un estudio considerando aspectos socioeconómicos y agroeconómicos en la zona de la cuenca del valle de Mala (localizada en el departamento de Lima, formando parte de las provincias de Cañete, Huarochirí y Yauyos).

De pescadores y agricultores: una historia local de la gente del valle de Chicama antes de 1565

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1995-01-01

Full Text Available DE PECHEURS ET AGRICULTEURS : UNE HISTOIRE LOCALE DES HABITANTS DE LA VALLEE DE CHICAMA AVANT 1565. Une transcription de la deuxième partie d'un manuscrit, daté de 1565 et publié ici, présente l'histoire orale de la vallée de Chicama, racontée par les chefs indigènes de l'époque de Guayna Capac. Une introduction au document donne des informations sur des rencontres entre Européens et indigènes sur l’implantation des Espagnols dans la vallée sur les conceptions différentes de la terre et de la tenure foncière et sur la dégradation du milieu naturel. Se presenta una transcripción de la segunda mitad de un manucristo de 1565 que cuenta la historia oral de los señores étnicos del valle de Chicama desde los tiempos de Guayna Capac. Una introducción al documento pone el manuscrito en su contexto histórico, hablando del encuentro entre los españoles y los naturales del asentamiento español del valle de los conceptos españoles e indígenas acerca de la tierra y la tenencia de dicho valle y la degradación del medio ambiente. ABOUT FISHERMEN AND AGRICULTURISTS: A LOCAL HISTORY OF THE PEOPLE IN CHICAMA'S VALLEY BEFORE 1565. A transcription of the second part of a manuscript, dated 1565 and published here, presents the oral history of the Valley of Chicama, as told by native lords, from the time of Guayna Capac. An introduction to the document provides information on the encounters between Europeans and natives Spanish settlement of the Valley conflicting conceptions of land and tenure and environmental degradation.

Environmental practices of the tourist companies in Valle de Bravo

International Nuclear Information System (INIS)

Hernandez Penaloza, Nadia; Zizumbo Villarreal, Lilia; Vargas Martinez, Elva Esther

2011-01-01

The present article analyzes the environmental practices of the social actors related to the tourist companies of the municipality of Valle de Bravo, Mexico State. The environmental practices were considered from the socioeconomic point of view, including not only the natural resources management, but also the social and economic environment. Considering the previous, using a methodological proposal based on the theory of complex systems, the effects on the above mentioned environments of this tourist destination were analyzed, allowing to holistically visualizing the situation that prevails towards the environmental caring performed by all the social actors of the locality. The results show a great weakness in the implementation of the above mentioned practices, due to the fact that nowadays these practices are imposed by the municipal government and are not an initiative of the actors of the tourist companies. For this reason, the conditions of environmental deterioration in Valle de Bravo are increasing. Based on the results, some recommendations are proposed for the implementation and improvement of environmental practices that contribute to the conservation and care of the environment.

Seven new species of Loneura Navás (Insecta: Psocodea: 'Psocoptera': Ptiloneuridae) from Valle del Cauca, Colombia.

Science.gov (United States)

Nieto, Julián Alexander Mendivil; Aldrete, Alfonso Neri García; Obando, Ranulfo González

2017-02-06

Seven species of Loneura from natural areas of Valle del Cauca, Colombia, are described and illustrated. The female of L. andina is described for the first time. Two additional species, known only from the National Natural Park Gorgona (Cauca), are also recorded in Valle del Cauca. The new species are assigned to the infrageneric groups known in the genus. An identification key to males of Loneura is included.

Campaniforme no funerario en la provincia de Toledo: el yacimiento de Las Vegas. De nuevo el Valle de Huecas

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Barroso Bermejo, Rosa

2015-06-01

Full Text Available This article presents the latest results of the excavations at the site of Las Vegas in Huecas (Toledo. The site is located in an open area, near a stream and at the foot of the Valle de las Higueras necropolis. It is buried by a considerable colluvial deposition and was detected by geophysical survey. The site lacks structures and is made up of a single archaeological layer: it is a secondary deposit, containing Bell Beaker pottery and metal. A 14C sample has dated it to the second half of the 3rd millennium BC. Ceramics are the most abundant remain from this deposit. Macroscopic and X-ray Fluorescence (FRX analysis of the ceramics indicates a local production, the fast formation of this deposit, and its long-term exposure on the surface. We suggest that it was formed by cleaning and maintenance activities carried out in a nearby occupational area. We suggest that settlement occurred in the valley bottom, with occupations whose ceramic productions differ from the ones found in funerary contexts.Presentamos los resultados de los sondeos del yacimiento de Las Vegas, Huecas (Toledo. Se trata de un área abierta, junto al arroyo y al pie de la necrópolis de Valle de las Higueras. Un fuerte depósito de coluvión sepulta el yacimiento. Sin evidencias en superficie, su detección se realizó mediante prospección geofísica. Carece de estructuras y está formado por un único estrato, un depósito secundario que contiene campaniforme Ciempozuelos y metal, con una fecha C14 de la 2ª mitad del III milenio a.C. La cerámica es el material más abundante. Su estudio macroscópico y mediante fluorescencia de rayos X (FRX avala su producción local, la rápida formación del depósito y su larga exposición en superficie. Planteamos que el depósito procede de la limpieza y mantenimiento de un área de ocupación anexa. El patrón de poblamiento parece seguir las tierras bajas del valle con ocupaciones cuyas producciones cerámicas difieren de las de los

Auqakuh Valles

Science.gov (United States)

2002-01-01

(Released 7 June 2002) The Science This ancient sinuous river channel, located near 30o N, 299o W (61o E), was likely carved by water early in Mars history. Auqakuh Valles cuts through a remarkable series of rock layers that were deposited and then subsequently eroded. This change from conditions favoring deposition to those favoring erosion indicates that the environment of this region has changed significantly over time. In addition, the different rock layers seen in this image vary in hardness, with some being relatively soft and easily eroded, whereas others are harder and resistant. These differences imply that these layers vary in their composition, physical properties, and/or degree of cementation, and again suggest that major changes have occurred during the history of this region. Similar differences occur throughout the southwest U.S., where hard rock layers, such as the limestones and sandstones in the Grand Canyon, form resistant cliffs, whereas softer mudstones are easily eroded to form broad slopes. The Martian layers, such as the smooth, dark-toned mesas visible in numerous places to the right (east) of the channel, were once continuous across the region. As these layers have eroded, they have produced a wide array of textures, from smooth surfaces, to knobby terrains, to the unusual lobate patterns seen in the upper right of the image. The most recent activity in the region appears to be the formation of mega-ripples by the wind. These ripples, spaced approximately 75 m apart, form perpendicular to the wind direction, and can be seen following the pattern of the channel floor as it curves through this region. This pattern shows that even this relatively small channel, which varies in width from about 500 to 750 m throughout this image, acts to funnel the wind down the channel. The Story Auqakuh Vallis, an ancient river channel that winds its way down the center of this image, is the 'fossil' remains of an earlier, probably more watery time in

Evolution of the sources of Moroccan volcanism during the Neogene

International Nuclear Information System (INIS)

El Azzouzi, M.; Griffiths, J.B.; Fourcade, S.; Hernandez, J.

1999-01-01

New major and trace element analyses, Sr-Nd isotopic data and 40 K- 40 Ar ages on Neogene and Quaternary lavas from Morocco lead to the conclusion that the observed temporal changes from calc-alkaline to transitional and finally magmatic activity reflect the contributions of distinct sources. According to our model, magmas originally derived from the melting of an European/Western Mediterranean-type asthenospheric mantle source interact during their ascent with either a sub-continental Roda - Beni Bousera -/type lithospheric mantle (alkaline magmas) or a lithospheric mantle containing a crystal component, and the overlying continental crust (calc-alkaline and, to a lesser extent, transitional magmas). (authors)

Uso de plaguicidas en un valle agrícola tecnificado en el noroeste de México

OpenAIRE

LEYVA MORALES, José Belisario; GARCÍA DE LA PARRA, Luz María; BASTIDAS BASTIDAS, Pedro de Jesús; ASTORGA RODRÍGUEZ, Jesús Efrén; BEJARANO TRUJILLO, Jorge; CRUZ HERNÁNDEZ, Alejandro; MARTÍNEZ RODRÍGUEZ, Irma Eugenia; BETANCOURT LOZANO, Miguel

2014-01-01

En el presente estudio se comparan dos procedimientos para conocer el uso de plaguicidas durante los ciclos otoño-invierno (O-I) 2011-2012 y primavera-verano (P-V) 2012 en el Valle de Culiacán, Sinaloa. A nivel nacional, este valle es una importante región agrícola tecnificada, productora de hortalizas y granos. Se analizaron las diferencias existentes en cuanto a cantidad total de ingrediente activo, según los registros del programa "Campo Limpio" y bitácoras de aplicación de varias empresas...

Estudio de factibilidad para la creación de un hotel en el Valle del Chota.

OpenAIRE

Bautista Espinosa, Carlos

2008-01-01

El presente proyecto contiene en el capítulo I, el estudio respecto de la factibilidad de implantar un Hotel & SPA en el Valle del Chota, parroquia Ambuquí, provincia de Imbabura, que brinde el servicio de hospedaje, distracción y relajación. La propuesta busca presentar un servicio turístico de relajación que atienda la demanda de alojamiento tanto interno como receptor que se dirige hacia el Valle del Chota en la parroquia de Ambuquí, adicionalmente se incluye el servicio de SPA con la ...

Perception of the general population in Ciudad Valles, San Luis Potosi regarding waste production in hairdressing salons

Directory of Open Access Journals (Sweden)

Juan José Maldonado-Miranda

2016-02-01

Full Text Available Hairdressing salons offer a wide range of services including treatments for hair and skin. However, these activities result in the production of residues that are improperly discharged into drainage, generating a negative impact on the environment. This study provides results of a first stage in a project regarding the analysis of waste disposal in hairdressing salons in the municipality of Ciudad Valles, San Luis Potosi, Mexico. Information gathering was conducted through a field work study by surveys given to workers in hairdressing salons in Ciudad Valles. The information presented in this study indicates that in hairdressing salons in Ciudad Valles there is no management plan for the management of waste that could be severely impacting the environment. The information presented here will be the basis for identifying priority areas for intervention, developing new research projects and setting new environmental policies. In addition, the results presented here can be extrapolated to many rural and urban areas all over Mexico.

Nuevos datos sobre la Huaca China, valle del Santa, Perú

Directory of Open Access Journals (Sweden)

2004-01-01

Full Text Available La présence Moche dans la vallée du Santa s’appuie sur l’existence de nombreux sites dont certains sont considérés comme des centres locaux importants. Huaca China est l’un de ces sites stratégiques dans la partie sud-ouest de la vallée. Des récoltes de surface combinées avec le nettoyage de six trous de pilleurs permettent l’identification d’une présence Moche et d’une forte occupation datant de l’Horizon Moyen. En plus de présenter une tombe de la culture Tanguche, les principales découvertes sont décrites dans l’optique de vérifier la présence Moche, son importance et la possibilité que les Moche aient construit les murailles entourant une petite plate-forme érigée sur le sommet de la colline. La presencia Moche en el valle del Santa se apoya en la existencia de numerosos sitios entre los cuales varios son considerados centros locales de importancia. Huaca China es uno de estos sitios estratégicos en la parte suroeste del valle. Las recolecciones de superficie y la limpieza de pozos de huaquero permiten la identificación de una presencia Moche y de una fuerte ocupación durante el Horizonte Medio. Además de presentar una sepultura de la cultura Tanguche, se describen los principales hallazgos con la finalidad de verificar la presencia Moche, su importancia, y se discute la posibilidad de que los Moche hayan construido las murallas que rodean una pequeña plataforma erigida en la cima de la colina donde se ubica este sitio. A Moche presence in the Santa Valley is supported by numerous sites, and the local centers have been identified. Huaca China in the south western portion of the valley is one of them. Surface collections combined with the cleaning of six looter’s pit allowed the identification of a Moche presence and also a strong Middle Horizon component. A Tanguche culture tomb is described and followed by the presentation of major cultural elements in order to establish the Moche presence, its importance, and

High resolution stratigraphy and paleoenvironmental changes in the southern North Sea during the Neogene : an integrated study of Late Cenozoic marine deposits from the northern part of the Dutch offshore area

NARCIS (Netherlands)

Kuhlmann, Gesa

2004-01-01

This thesis is the result of a multidisciplinary study on the prograding marine Neogene sedimentary succession of the southern North Sea Basin. To date, sediment material available from the Neogene North Sea is very scarce. Its location between 400 and 1500 m below the seabed in the depocentre of

High resolution stratigraphy and paleoenvironmental changes in the southern North Sea during the Neogene : An integrated study of Late Cenozoic marine deposits from the northern part of the Dutch offshore area

NARCIS (Netherlands)

Kuhlmann, G.

2004-01-01

This thesis is the result of a multidisciplinary study on the prograding marine Neogene sedimentary succession of the southern North Sea Basin. To date, sediment material available from the Neogene North Sea is very scarce. Its location between 400 and 1500 m below the seabed in the depocentre of

De la Vallee Poussin problem in the kernel of the convolution operator on the half-plane

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Valentin V. Napalkov

2015-06-01

Full Text Available We consider the multipoint de la Vallee Poussin (interpolational problem in the half-plane $D$, $D=ż  :  \\mathop{\\mathrm{Re}} z0\\}$. Let $\\psi(z\\in H(D$; $\\mu_1$, $\\mu_2$, $\\ldots \\in D$ be the positive zero points of this function and let the boundary of domain $D$ contain their limit. Also, we assume that $\\mu_k$ is of $s_k$ multiplicity, $k=1, 2, …$. Let us set $M_{\\varphi}$ an operator of convolution with the characteristic function $\\varphi(z$. Taking an arbitrary sequence $a_{kj},$ $j=0, 1, \\ldots, s_k-1$ we should ask: is there a function $u(z \\in \\mathop{\\mathrm{Ker}}M_\\varphi$ that provides the relation $u^{(j}(\\mu_{k}=a_{kj},$ $j=0, 1,…,s_k-1$? We assume the operator characteristic function to be of completely regular growth. The solvability conditions for the multipoint de la Vallée Poussin problem in the half-plain and in the bounded convex domains are obtained.

Late Neogene leaf assemblage from Bełchatów Lignite Mine (central Poland

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Worobiec Grzegorz

2014-12-01

Full Text Available Leaf macroremains collected in the Bełchatów Lignite Mine (central Poland were investigated. The fossil assemblage consists of leaves of Acer, Betula, Carpinus, Dicotylophyllum, Fagus, ?Magnolia, “Parrotia”, Pinus, Quercus, and Zelkova. Mesophytic (zonal elements dominate, with admixture of riparian (azonal leaf taxa. The floristic composition points to late Neogene (late Miocene to late Pliocene age and suggests favourable temperate climate with mild winters.

El polen de las mieles del valle de Río Negro, provincia fitogeográfica del monte (Argentina

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María C. Tellería

2000-01-01

Full Text Available Tellería, M. C. & Forcone, A. 2000. El polen de las mieles del valle de Río Negro, provinciafitogeográfica del monte (Argentina. Darwiniana 38(3-4: 273-277.Se realizó el análisis palinológico de 41 muestras de miel del valle de Río Negro. El contenido polínicode las muestras fue acetolizado e identificado por comparación con una colección de polen de referencia.Del total de muestras examinadas, 26 fueron mixtas y las restantes monoflorales de: Tamarix gallica (8muestras, Eucalyptus sp. (2 muestras, Melilotus sp. (1 muestra, Centaurea sp. (1 muestra, Prosopissp. (1 muestra, Brassicaceae (1 muestra y Monttea aphylla (1 muestra. Estas mieles pueden diferenciar-se de aquellas que se producen en el valle inferior del río Chubut, en la misma región fitogeográfica

Petrogenesis of Neogene basaltic volcanism associated with the Lut block, eastern Iran: Implication for tectonic and metallogenic evolution

Science.gov (United States)

Saadat, Saeed

This dissertation presents petrochemical data concerning Neogene olivine basalts erupted both along the margins and within the micro-continental Lut block, eastern Iran, which is a part of the active Alpine-Himalayan orogenic belt. These data demonstrate the following: (1) Basalts that erupted from small monogenetic parasitic cones around the Bazman stratovolcano, Makran arc area, in the southern Lut block, are low-Ti sub-alkaline olivine basalts. Enrichments of LILE relative to LREE, and depletions in Nb and Ta relatively to LILE, are similar to those observed for other convergent plate boundary arc magmas around the world and suggest that these basalts formed by melting of subcontinental mantle modified by dehydration of the subducted Oman Sea oceanic lithosphere. (2) Northeast of Iran, an isolated outcrop of Neogene/Quaternary alkali olivine basalt, containing mantle and crustal xenoliths, formed by mixing of small melt fractions from both garnet and spinel-facies mantle. These melts rose to the surface along localized pathways associated with extension at the junction between the N-S right-lateral strike-slip faults and E-W left-lateral strike slip faults. The spinel-peridotite mantle xenoliths contained in the basalts, which equilibrated in the subcontinental lithosphere at depths of 30 to 60 km and temperatures of 965°C to 1065°C, do not preserve evidence of extensive metasomatic enrichment as has been inferred for the mantle below the Damavand volcano further to the west in north-central Iran. (3) Neogene mafic rocks within the central Lut block represent the last manifestation of a much more extensive mid-Tertiary magmatic event. These basalts formed from both OIB-like asthenosphere and subcontinental lithosphere which preserved chemical characteristics inherited from mid-Tertiary subduction associated with the collision of the Arabian with the Eurasian plate and closing of the Neotethys Ocean. Neogene/Quternary alkali olivine basalts erupted mainly along

New allocyclic dimensions in a prograding carbonate bank: Evidence for eustatic, tectonic, and paleoceanographic control (late Neogene, Bahamas)

Science.gov (United States)

Lidz, B.H.; McNeill, D.F.

1997-01-01

The deep-sea record, examined recently for the first time in a shallow-depocenter setting, has unveiled remarkable evidence for new sedimentary components and allocyclic complexity in a large, well-studied carbonate bank, the western Great Bahama Bank. The evidence is a composite foraminiferal signature - Paleocene to early Miocene (allogenic or reworked) and late Miocene to late Pliocene (host) planktic taxa, and redeposited middle Miocene shallow benthic faunas. Ages of the oldest and youngest planktic groups range from ??? 66 to ??? 2 Ma. The reworked and redeposited taxa are a proxy for significant sediment components that otherwise have no lithofacies or seismic resolution. The composite signature, reinforced by a distinctive distribution of the reworked and redeposited faunas, documents a much more complex late Neogene depositional system than previously known. The system is more than progradational. The source sequences that supplied the constituent bank-margin grains formed at different water depths and over hundreds of kilometers and tens of millions of years apart. New evidence from the literature and from data obtained during Ocean Drilling Program (OOP) Leg 166 in the Santaren Channel (Bahamas) support early interpretations based on the composite fossil record and provide valuable new dimensions to regional allocyclicity. The middle Miocene taxa were confined to the lower part of the section by the latest Miocene-earliest Pliocene(?) lowstand of sea level. An orderly occurrence of the allogenic taxa is unique to the global reworked geologic record and appears to have been controlled by a combination of Paleogene-early Neogene tectonics at the source, eustatic changes, and late Neogene current activity at the source and across the bank. The allogenic taxa expand the spatial and temporal range of information in the northern Bahamas by nearly an order of magnitude. In essence, some of the major processes active in the region during ??? 64 m.y. of the

Formación del patrimonio gastronómico del Valle de Toluca, México

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Alejandro Tonatiuh Romero Contreras

2011-01-01

Full Text Available Se describe la formación de la cocina patrimonial de la región de Toluca como primer paso para su investigación culinaria. Se utilizó información etnohistórica de primera mano (cronistas y la consulta de libros, recetarios, tesis y otros documentos, relacionándolos con las características ambientales y culturales del Valle de Toluca. Se identificaron las especies animales y vegetales, así como las prácticas agrícolas-culinarias que trajeron consigo los españoles y su fusión con sus similares locales, lo que produjo el mestizaje gastronómico en el Valle de Toluca expresado en sus platillos patrimoniales: barbacoas, embutidos, moles, tamales, dulces y bebidas tradicionales.

Long-term fluid circulation in extensional faults in the central Catalan Coastal Ranges: P-T constraints from neoformed chlorite and K-white mica

Science.gov (United States)

Cantarero, Irene; Lanari, Pierre; Vidal, Olivier; Alías, Gemma; Travé, Anna; Baqués, Vinyet

2014-01-01

The neoformation of chlorite and K-white mica in fault rocks from two main faults of the central Catalan Coastal Ranges, the Vallès and the Hospital faults, has allowed us to constrain the P-T conditions during fault evolution using thermodynamic modeling. Crystallization of M1 and M2 muscovite and microcline occured as result of deuteric alteration during the exhumation of the pluton (290 °C > T > 370 °C) in the Permian. After that, three tectonic events have been distinguished. The first tectonic event, attributed to the Mesozoic rifting, is characterized by precipitation of M3 and M4 phengite together with chlorite and calcite C1 at temperatures between 190 and 310 °C. The second tectonic event attributed to the Paleogene compression has only been identified in the Hospital fault with precipitation of low-temperature calcite C2. The shortcut produced during inversion of the Vallès fault was probably the responsible for the lack of neoformed minerals within this fault. Finally, the third tectonic event, which is related to the Neogene extension, is characterized in the Vallès fault by a new generation of chlorite, associated with calcite C4 and laumontite, formed at temperatures between 125 and 190 °C in the absence of K-white mica. Differently, the Hospital fault is characterized by the precipitation of calcite C3 during the syn-rift stage at temperatures around 150 °C and by low-temperature fluids precipitating calcites C5, C6 and PC1 during the post-rift stage. During the two extensional events (Mesozoic and Neogene), faults acted as conduits for hot fluids producing anomalous high geothermal gradients (50 °C/km minimum).

Evolution of basin architecture in an incipient continental rift: the Cenozoic Most Basin, Eger Graben (Central Europe)

Czech Academy of Sciences Publication Activity Database

Rajchl, M.; Uličný, David; Grygar, R.; Mach, K.

2009-01-01

Roč. 21, č. 3 (2009), s. 269-294 ISSN 0950-091X R&D Projects: GA AV ČR IAA3012705; GA ČR GA205/01/0629; GA ČR(CZ) GA205/06/1823 Institutional research plan: CEZ:AV0Z30120515 Keywords : Cenozoic Most Basin * continental rift * Eger Graben Subject RIV: DB - Geology ; Mineralogy Impact factor: 2.161, year: 2009

New evidence for a magmatic influence on the origin of Valles Marineris, Mars

Science.gov (United States)

Dohm, J.M.; Williams, J.-P.; Anderson, R.C.; Ruiz, J.; McGuire, P.C.; Komatsu, G.; Davila, A.F.; Ferris, J.C.; Schulze-Makuch, D.; Baker, V.R.; Boynton, W.V.; Fairen, A.G.; Hare, T.M.; Miyamoto, H.; Tanaka, K.L.; Wheelock, S.J.

2009-01-01

In this paper, we show that the complex geological evolution of Valles Marineris, Mars, has been highly influenced by the manifestation of magmatism (e.g., possible plume activity). This is based on a diversity of evidence, reported here, for the central part, Melas Chasma, and nearby regions, including uplift, loss of huge volumes of material, flexure, volcanism, and possible hydrothermal and endogenic-induced outflow channel activity. Observations include: (1) the identification of a new > 50??km-diameter caldera/vent-like feature on the southwest flank of Melas, which is spatially associated with a previously identified center of tectonic activity using Viking data; (2) a prominent topographic rise at the central part of Valles Marineris, which includes Melas Chasma, interpreted to mark an uplift, consistent with faults that are radial and concentric about it; (3) HiRISE-identified landforms along the floor of the southeast part of Melas Chasma that are interpreted to reveal a volcanic field; (4) CRISM identification of sulfate-rich outcrops, which could be indicative of hydrothermal deposits; (5) GRS K/Th signature interpreted as water-magma interactions and/or variations in rock composition; and (6) geophysical evidence that may indicate partial compensation of the canyon and/or higher density intrusives beneath it. Long-term magma, tectonic, and water interactions (Late Noachian into the Amazonian), albeit intermittent, point to an elevated life potential, and thus Valles Marineris is considered a prime target for future life detection missions. ?? 2008 Elsevier B.V.

Applying hydrology to land management on the Valles Caldera National Preserve

Science.gov (United States)

Robert R. Parmenter

2009-01-01

Since 2004, the Valles Caldera National Preserve (VCNP) in the Jemez Mountains of northern New Mexico has hosted extensive field hydrology research by scientists from the Center for Sustainability of semi- Arid Hydrology and Riparian Areas (SAHRA) at the University of Arizona. With the development of a detailed hydrologic understanding of VCNP's climate, geology,...

Kapital ja sotsiaalsed vajadused / Robin Blackburn ; ref. Valle-Sten Maiste

Index Scriptorium Estoniae

Blackburn, Robin

2006-01-01

Autori väitel püüdleb EL vaid siseturu laiendamise poole, pakkumata sotsiaalset turvalisust ja maksude ühtlustamist. Euroopa vajab märgatavalt efektiivsemaid korporatsioonide maksustamise viise, millele järgneks sotsiaalsete fondide võrgustiku rajamine. Sotsiaalsete fondide kaudu ei jaotataks ainult rikkust ümber, vaid investeeritaks ka loodus- ja tööskeskkonda. Vt. samas ka Valle-Sten Maiste art. "Naabrist rohkem pappi"

Perspectives on managing multi-cultural landscapes: Use, access, and fire/fuels management attitudes and preferences of user groups concerning the Valles Caldera National Preserve (VCNP) and adjacent areas

Science.gov (United States)

Kurt F. Anschuetz

2014-01-01

The Valles Caldera National Preserve (VCNP), which consists of a large, 1.2- to 1.6-million-year-old volcanic caldera, forms the heart of the Jemez Mountains in north-central New Mexico (Figure 1). Known as the Valles Caldera, this bowl-shaped hollow is an especially treasured place within this beloved mountainous landscape for many residents of the region. Its valles...

Gravity evidence for shaping of the crustal structure of the Ameca graben (Jalisco block northern limit). Western Mexico

Science.gov (United States)

Alatorre-Zamora, Miguel Angel; Campos-Enríquez, José Oscar; Fregoso-Becerra, Emilia; Quintanar-Robles, Luis; Toscano-Fletes, Roberto; Rosas-Elguera, José

2018-03-01

The Ameca tectonic depression (ATD) is located at the NE of the Jalisco Block along the southwestern fringe of the NW-SE trending Tepic-Zacoalco Rift, in the west-central part of the Trans-Mexican Volcanic Belt, western Mexico. To characterize its shallow crustal structure, we conducted a gravity survey based on nine N-S gravity profiles across the western half of the Ameca Valley. The Bouguer residual anomalies are featured by a central low between two zones of positive gravity values with marked gravity gradients. These anomalies have a general NW-SE trend similar to the Tepic-Zacoalco Rift general trend. Basement topography along these profiles was obtained by means of: 1) a Tsuboi's type inverse modeling, and 2) forward modeling. Approximately northward dipping 10° slopes are modeled in the southern half, with south tilted down faulted blocks of the Cretaceous granitic basement and its volcano-sedimentary cover along sub-vertical and intermediate normal faults, whereas southward dipping slopes of almost 15° are observed at the northern half. According to features of the obtained models, this depression corresponds to a slight asymmetric graben. The Ameca Fault is part of the master fault system along its northern limit. The quantitative interpretation shows an approximately 500 to 1100 m thick volcano-sedimentary infill capped by alluvial products. This study has several implications concerning the limit between the Jalisco Block and the Tepic-Zacoalco Rift. The established shallow crustal structure points to the existence of a major listric fault with its detachment surface beneath the Tepic-Zacoalco Rift. The Ameca Fault is interpreted as a secondary listric fault. The models indicate the presence of granitic bodies of the Jalisco Block beneath the TMVB volcanic products of the Tepic-Zacoalco rift. This implies that the limit between these two regional structures is not simple but involves a complex transition zone. A generic model suggests that the

Contrasting neogene denudation histories of different structural regions in the transantarctic mountains rift flank constrained by cosmogenic isotope measurements

NARCIS (Netherlands)

Wateren, F.M. van der; Dunai, T.J.; Balen, R.T. van; Klas, W.; Verbers, A.L.L.M.; Passchier, S.; Herpers, U.

1999-01-01

Separate regions within the Transantarctic Mountains, the uplifted flank of the West Antarctic rift system, appear to have distinct Neogene histories of glaciation and valley downcutting. Incision of deep glacial outlet valleys occurred at different times throughout central and northern Victoria

Stratigraphy and mineralogy of Candor Mensa, West Candor Chasma, Mars: Insights into the geologic history of Valles Marineris

Science.gov (United States)

Fueten, F.; Flahaut, J.; Stesky, R.; Hauber, E.; Rossi, A. P.

2014-02-01

Candor Mensa, an interior layered deposit (ILD) in Valles Marineris, Mars, consists of two stratigraphically distinct units, the lower of which comprises the bulk of the mensa. This lower unit is approximately 5 km thick and composed of parallel layers, 4 to 14 m in thickness and associated with monohydrated sulfates. The lower unit is disconformably overlain by an upper unit composed of thinner (ancestral basins into the current geometry of Valles Marineris chasmata and that it was possible to form hydrated minerals after this event.

POLÍTICA PÚBLICA AMBIENTAL Y AMBIENTE EN EL VALLE DEL CAUCA, 1991-2010

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Álvaro Quiceno Martínez

2010-01-01

Full Text Available La política pública ambiental en el Valle del Cauca, a partir de 1991, va en contravía de la conservación ambiental al enfatizar en el crecimiento económico, la generación de plusvalía y la ampliación de la tasa de ganancia. Para la realización de esta investigación se adoptó como herramienta metodológica la revisión bibliográfica. Se halló que la política pública ambiental en el Valle se ha orientado a subsidiar monetaria, ecológica, ambiental y socialmente al sector cañicultor. Se concluye que dicha política ha contribuido al desequilibrio ecológico y al deterioro ambiental.

Neogene palaeochannel deposits in Sudan - Remnants of a trans-Saharan river system?

Science.gov (United States)

Bussert, Robert; Eisawi, Ali A. M.; Hamed, Basher; Babikir, Ibrahim A. A.

2018-05-01

The start of Nile-type trans-Saharan drainage systems in NE Africa during the Cenozoic is disputed. Stratigraphical and sedimentological data in Egypt are partly in conflict with the uplift history of potential source areas of water and sediment in East Africa. Here, we investigate outcrops of the Wadi Awatib Conglomerate in Sudan that provide the first evidence of northerly flowing Neogene rivers in the region. Dimension and relief of basal erosion surfaces, overall geometry of deposits and palaeocurrent indicators demonstrate that the deposits represent the fill of northward-oriented incised valleys. The conglomerates were deposited in deep gravel-bed rivers, by hyperconcentrated flows, tractions carpets and gravel bars, primarily during heavily sediment-laden floods of probably monsoonal origin. Stratigraphical and geomorphological relationships show that the deposits are between Eocene and Pliocene in age. Considering the structural history of the region and periods in the Cenozoic with palaeoclimatic conditions suitable for the production and transport of gravels, we hypothesize that the dramatic base-level fall during the Late Miocene Messinian salinity crisis in combination with a favorable palaeoclimate caused the incision of valleys and their subsequent filling with conglomerates. Sea-level change in the Mediterranean Sea and headward erosion of streams that were connected to the Egyptian Nile might have been the primary cause of valley incision and deposition of conglomerates, despite a location far inland from the coastline. We suggest that the deposits document a relatively young Neogene (Messinian to early Pliocene) trans-Saharan river system unrelated to uplift of the Ethiopian Plateau.

Trace element chemistry and textures of low-temperature pyrites associated with shallow fossil subsurface geothermal discharge in the Eger Graben, northwestern Bohemia

Czech Academy of Sciences Publication Activity Database

Zachariáš, J.; Adamovič, Jiří; Langrová, Anna

2006-01-01

Roč. 37, 29 (2006), s. 237-239 ISSN 0032-6267 R&D Projects: GA AV ČR IAA3013302 Institutional research plan: CEZ:AV0Z30130516 Keywords : pyrite * geothermal fluids * Eger Graben Subject RIV: DB - Geology ; Mineralogy

Observación Electoral: Experiencia de la MOE Regional Valle del Cauca, Elecciones Nacionales de Colombia 2010

OpenAIRE

Escobar Higuera, Katherine

2013-01-01

En el presente artículo se reseña la experiencia de Observación electoral en el departamento del Valle del Cauca, por parte de la Misión de Observación Electoral MOE regional Valle. Con el propósito de visibilizar el trabajo de una red de organizaciones y personas que han tomado iniciativa en el mejoramiento de un proceso importante para el sistema democrático colombiano, las elecciones. Al reseñar esta experiencia, se espera sea referente de una acción de participación política desde las org...

Genomic characterisation of Arachis porphyrocalyx (Valls & C.E. Simpson, 2005) (Leguminosae): multiple origin of Arachis species with x = 9

Science.gov (United States)

Celeste, Silvestri María; Ortiz, Alejandra Marcela; Robledo, Germán Ariel; Valls, José Francisco Montenegro; Lavia, Graciela Inés

2017-01-01

Abstract The genus Arachis Linnaeus, 1753 comprises four species with x = 9, three belong to the section Arachis: Arachis praecox (Krapov. W.C. Greg. & Valls, 1994), Arachis palustris (Krapov. W.C. Greg. & Valls, 1994) and Arachis decora (Krapov. W.C. Greg. & Valls, 1994) and only one belongs to the section Erectoides: Arachis porphyrocalyx (Valls & C.E. Simpson, 2005). Recently, the x = 9 species of section Arachis have been assigned to G genome, the latest described so far. The genomic relationship of Arachis porphyrocalyx with these species is controversial. In the present work, we carried out a karyotypic characterisation of Arachis porphyrocalyx to evaluate its genomic structure and analyse the origin of all x = 9 Arachis species. Arachis porphyrocalyx showed a karyotype formula of 14m+4st, one pair of A chromosomes, satellited chromosomes type 8, one pair of 45S rDNA sites in the SAT chromosomes, one pair of 5S rDNA sites and pericentromeric C-DAPI+ bands in all chromosomes. Karyotype structure indicates that Arachis porphyrocalyx does not share the same genome type with the other three x = 9 species and neither with the remaining Erectoides species. Taking into account the geographic distribution, morphological and cytogenetic features, the origin of species with x = 9 of the genus Arachis cannot be unique; instead, they originated at least twice in the evolutionary history of the genus. PMID:28919947

Calidad de aguas naturales y residuales en el sistema hidrográfico Valle del Mezquital, Hidalgo México.

OpenAIRE

Barrios Castillo, Isaac Mateo

2014-01-01

Actualmente se ha usado prácticamente toda el agua disponible para satisfacer los requerimientos de los diferentes cultivos que se explotan en la agricultura bajo riego. Cada vez más se utilizan hasta el límite las aguas superficiales y subterráneas de la más variada composición química y concentración de sales. En México, se riegan aproximadamente 180,000 ha en diferentes lugares del Valle del Mezquital con aguas residuales urbano-industriales que derivan de la zona metropolitana del Valle d...

DIAGNÓSTICO Y PROPUESTA PARA UNA GESTIÓN INTEGRAL DEL RIESGO EN EL VALLE DE ABURRA: RED RIESGOS

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ARISTIZÁBAL EDIER; VARGAS RICHARD

2010-01-01

A partir del análisis de la situación organizacional de las diferentes instituciones en el Valle de Aburrá frente a la reducción de desastres y emergencias asociadas con los fenómenos de origen natural y antrópico, el Área Metropolitana del Valle de Aburrá, como autoridad ambiental y entidad planificadora, hace una propuesta que pretende articular todas las entidades, organizaciones e instituciones públicas y privadas hacia una gestión integral del riesgo, y la cual denominó: Red para la Gest...

3D geological modeling of the transboundary Berzdorf-Radomierzyce basin in Upper Lusatia (Germany/Poland)

Science.gov (United States)

Woloszyn, Iwona; Merkel, Broder; Stanek, Klaus

2017-07-01

The management of natural resources has to follow the principles of sustainable development. Therefore, before starting new mining activities, it should be checked, whether existing deposits have been completely exploited. In this study, a three-dimensional (3D) cross-border geologic model was created to generalize the existing data of the Neogene Berzdorf-Radomierzyce basin, located in Upper Lusatia on the Polish-German border south of the city of Görlitz-Zgorzelec. The model based on boreholes and cross sections of abandoned and planned lignite fields was extended to the Bernstadt and Neisse-Ręczyn Graben, an important tectonic structure at the southern rim of the basin. The partly detailed stratigraphy of Neogene sequences was combined to five stratigraphic units, considering the lithological variations and the main tectonic structures. The model was used to check the ability of a further utilization of the Bernstadt and Neisse-Ręczyn Graben, containing lignite deposits. Moreover, it will serve as a basis for the construction of a 3D cross-border groundwater model, to investigate the groundwater flow and transport in the Miocene and Quaternary aquifer systems. The large amount of data and compatibility with other software favored the application of the 3D geo-modeling software Paradigm GOCAD. The results demonstrate a very good fit between model and real geological boundaries. This is particularly evident by matching the modeled surfaces to the implemented geological cross sections. The created model can be used for planning of full-scale mining operations in the eastern part of the basin (Radomierzyce).

Proyecto MeCIN: Alto Valle de Río Negro, Argentina MeCIN Project: alto Valle of Rio negro, Argentina

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Alberto L Flores

2006-12-01

Full Text Available Este trabajo presenta los resultados obtenidos durante el experimento de campo MeCIN (Mediciones de la Capa de Inversión Nocturna cuyo objetivo fue estudiar el comportamiento del viento, la temperatura del aire y la evolución del enfriamiento en los valles de los ríos Neuquén, Limay y Negro en noches con inversión térmica en las primaveras de los años 1992 al 1997. Las situaciones sinópticas que propiciaron los intensos efectos radiativos nocturnos fueron asociadas con un anticiclón migratorio postfrontal en 1000 hPa y un eje de vaguada en 500 hPa. Los gradientes verticales de temperatura alcanzaron valores medios entre 0,26 °C/m en el valle del río Neuquén y 0,14 °C/m en el del Negro. El tope de la inversión térmica, en promedio, se ubicó a más de 30 m. Las mediciones de los perfiles de velocidad del viento mostraron un patrón de dos capas: una capa inferior sin movimiento y otra superior con velocidades en promedio entre 2,9 m/s y 4,0 m/s. El enfriamiento nocturno fue superior en la zona de chacras y menor en cercanías del río y sobre la meseta. La temperatura del aire durante la noche fue menor en el valle que en la meseta, dependiendo de su altura.This paper presents the results of field experience MeCIN (Measurements of the Nocturnal Inversion Layer. The project was performed to study the characteristics of wind, air temperature and the evolution of nocturnal cooling in the Neuquén, Limay, and Negro river valleys during nighttime with thermal inversion in the layer near ground, between 1992 and 1997 spring seasons. The mean synoptic situations that favored the nocturnal radiative effects were associated with migratory postfrontal 1000 hPa anticyclones and a though axis in 500 hPa. The mean vertical gradient of air temperature was 0,26 °C/m in the Neuquén river valley and 0,14 °C/m in the Negro river valley. The top of the thermal inversion, on the average, was located above 30 m. The wind speed profile presented two

Denudation and uplift of the Mawson Escarpment (eastern Lambert Graben, Antarctica) as indicated by apatite fission track data and geomorphological observation

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Lisker, F.; Gibson, H.; Wilson, C.J.; Läufer, A.

2007-01-01

Analysis of three vertical profiles from the southern Mawson Escarpment (Lambert Graben) reveals apatite fission track (AFT) ages ranging from 102±20 to 287±23 Ma and mean lengths of 12.2 to 13.0 μm. Quantitative thermal histories derived from these data consistently indicate onset of slow cooling below 110°C began sometime prior to 300 Ma, and a second stage of rapid cooling from paleotemperatures up to ≤100°C to surface temperatures occurred in the Late Cretaceous – Paleocene. The first cooling phase refers to Carboniferous – Jurassic basement denudation up to 5 km associated with the initial rifting of the Lambert Graben. The presence of the ancient East Antarctic Erosion Surface and rapid Late Cretaceous – Paleocene cooling indicate a second denudational episode during which up to 4.5 km of sedimentary cover rocks were removed, and that is likely linked to the Cretaceous Gondwana breakup between Antarctica and India and subsequent passive continental margin formation.

An updated biostratigraphy for the late Aragonian and Vallesian of the Valles Basin (Catalonia)

Energy Technology Data Exchange (ETDEWEB)

Casanovas-Vilar, I.; Garces, M.; Dam, J. van; Garcia-Paredes, I.; Robles, J.M.; Alba, D.M.

2016-07-01

The Valles Basin (Catalonia, Spain) is a classical area for the study of the Miocene land mammal faunas and includes one of the densest and most continuous records in Eurasia. Furthermore, it is the type area for the Vallesian European land mammal age. After decades of study a huge amount of bio- and magnetostratigraphic data have been collected, allowing an unprecedented dating accuracy. Here we provide an updated local biostratigraphy for the late Aragonian, Vallesian and Turolian of the Vallès-Penedès Basin. This new biostratigraphic scheme is almost exclusively based on fossil rodents, which are the most abundant and one of the best known mammal orders in the area. Our proposal represents a significant refinement compared to previous attempts and provides a formal diagnosis and description of each zone, as well as clear definition of boundaries and a reference locality and section. The chronology of zone boundaries and main bioevents is based on detailed magnetostratigraphic data. The defined biozones allow for the correlation of the sites without associated magnetostratigraphical data. Finally, the correlation of the Vallès-Penedès local zones with other detailed local biostratigraphies, such as those of the Calatayud-Montalbán and Teruel basins (east-central Spain) is discussed. The sequence and chronology of the main bioevents is roughly comparable, although the rodent succession and the structure of the assemblage show important differences between these areas. (Author)

Fauna anfibia del valle de sibundoy, putumayo-colombia

OpenAIRE

MUESES-CISNEROS, JONH JAIRO

2012-01-01

La fauna Amphibia del Valle de Sibundoy consta de 32 especies agrupadas en dos órdenes, cinco familias y siete géneros. De éstas, cinco son especies nuevas cuya descripción se encuentra en proceso. Se amplía el límite altitudinal de otras siete y se presentan tres más para ser incluidas en la lista de anfibios de Colombia. A pesar de que en el lugar se han realizado colectas herpetológicas desde finales de los años sesenta, este estudio es el primero que se realiza en el Putumayo (uno de los ...

Geological Mapping and Investigation into a Proposed Syn-rift Alluvial Fan Deposit in the Kerpini Fault Block, Greece.

OpenAIRE

Hadland, Sindre

2016-01-01

Master's thesis in Petroleum geosciences engineering The Kerpini Fault Block is located in the southern part of the Gulf of Corinth rift system. The rift system consists of several east-west orientated half-grabens with associated syn-rift sediments. Kerpini Fault Block is one of the southernmost half-grabens within the rift systems, and is composed of several different stratigraphic units. The stratigraphic framework consists of a complex interaction of several stratigraphic units. One of...

Hydrology of the Upper-Garonne basin (Valle de Arán, Spain)

NARCIS (Netherlands)

Rijckborst, H.

1967-01-01

The runoff in the Valle de Arán, which is a steep and high mountain basin in the Pyrenees, consists essentially of baseflow, and fast runoff is only a minor phenomenon. The baseflow is related to areas of scree and forest, and the percentage of the precipitation which contributes to the fast runoff,

Mismi y Huarancante: nevados sagrados del Valle de Colca.

OpenAIRE

Ceruti, María Constanza

2013-01-01

El presente trabajo hace referencia a ascensiones efectuadas por la autora a las cimas de los montes Mismi (5596 m) y Huarancante (5360 m), en el sur de Perú. Ambas montañas ostentan evidencias de sitios rituales de altura de probable filiación Inca en avanzado estado de destrucción por eventos de huaqueo que se remontan a fines de la década del setenta. Al igual que otros nevados que flanquean al valle de Colca, el Huarancante y el Mismi siguen ...

Variabilidad genética de Hartón del Valle mediante RAM Genetic variability of Harton del Valle by RAM

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Ana M Piedrahíta

2008-01-01

Full Text Available El Hartón del Valle (HV hace parte de las siete razas criollas de ganado bovino colombiano y de acuerdo con los criterios de la FAO está considerado como vulnerable. Para estudiar su variabilidad genética fueron muestreados 33 individuos HV y tres animales de la raza Holstein, como control externo. Se extrajo ADN utilizando el método de Salting Out y las muestras fueron analizadas mediante la técnica molecular RAM (Randon amplified microsatellites. Se utilizaron los cebadores CGA, CCA, TG, y CT. El valor promedio de heterocigosidad esperada fue de 0.26 y el F ST fue 0.39 ± 0.03. Con el índice de Dice-Nei Li y agrupando con el método UPGMA se distinguieron dos grupos: uno integrado por dos hatos de conservación y el otro por cuatro fincas que han compartido reproductores.Harton del Valle (HV breed belong to the seven Creole breeds of the Colombian bovine livestock, according to FAO criteria it is considered as vulnerable. To study its genetical variability, 33 HV animals and three and 3 animals of Holstein breed as a external control were sampled. Simples of DNA were isolated using the Salting Out method and RAM (Random amplified microsatellites technique was used. CGA, CCA, TG and CT primers were used. The mean value of expected heterocigozity was 0.26 and F ST fue 0.39 ± 0.03. Using Dice-Nei Li index and UPGMA clustering method, two groups were distinguished: the first one integrated for two conservation herds and other one by tour faros that have been sharing breeding bulls.

Evolution of organic carbon burial in the Global Ocean during the Neogene

Science.gov (United States)

LI, Z.; Zhang, Y.

2017-12-01

Although only a small fraction of the organic carbon (OC) that rains from surface waters is eventually buried in the sediments, it is a process that controls the organic sub-cycle of the long-term carbon cycle, and the key for atmospheric O2, CO2 and nutrient cycling. Here we constrain the spatiotemporal variability of OC burial by quantifying the total organic carbon (TOC) mass accumulation rate (MAR) over the Neogene (23.0-2.6 Ma) by compiling the TOC, age model and sediment density data from sites retrieved by the Deep Sea Drilling Program, Ocean Drilling Program, and Integrated Ocean Drilling Program. We screened all available sites which yielded 80 sites with adequate data quality, covering all major ocean basins and sedimentary depositional environments. All age models are updated to the GTS 2012 timescale so the TOC MAR records from different sites are comparable. Preliminary results show a clear early Miocene peak of OC burial in many sites related to high sediment flux which might reflect the orogenic uplift and/or glacier erosion. Places that receive high influx of terrigenous inputs become "hotspots" for Neogene burial of OC. At "open ocean" sites, OC burial seems to be more impacted by marine productivity changes, with a pronounced increase during the middle Miocene "Monterey Formation" and late Miocene - early Pliocene "Biogenic Bloom". Upon the completion of the data collection, we will further explore the regional and global OC burial in the context of tectonic uplift, climate change and the evolution of primary producers and consumers during the last 23 million years of Earth history.

Asymmetric lithosphere as the cause of rifting and magmatism in the Permo-Carboniferous Oslo Graben, in Permo-Carboniferous Rifting and Magmatism in Europe.

NARCIS (Netherlands)

Pascal Candas, C.; Cloetingh, S.A.P.L.; Davies, G.R.

2004-01-01

Compared to other Permo-Carboniferous rift basins of NW Europe, the Oslo Graben has two distinct characteristics. First, it initiated inside cold and stable Precambrian lithosphere, whereas most Permo-Carboniferous basins developed in weaker Phanerozoic lithosphere, and second, it is characterized

Limited role for thermal erosion by turbulent lava in proximal Athabasca Valles, Mars

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Cataldo, Vincenzo; Williams, David A.; Dundas, Colin M.; Kestay, Laszlo P.

2015-01-01

The Athabasca Valles flood lava is among the most recent (Mars and was probably emplaced turbulently. The Williams et al. (2005) model of thermal erosion by lava has been applied to what we term “proximal Athabasca,” the 75 km long upstream portion of Athabasca Valles. For emplacement volumes of 5000 and 7500 km3and average flow thicknesses of 20 and 30 m, the duration of the eruption varies between ~11 and ~37 days. The erosion of the lava flow substrate is investigated for three eruption temperatures (1270°C, 1260°C, and 1250°C), and volatile contents equivalent to 0–65 vol % bubbles. The largest erosion depths of ~3.8–7.5 m are at the lava source, for 20 m thick and bubble-free flows that erupted at their liquidus temperature (1270°C). A substrate containing 25 vol % ice leads to maximum erosion. A lava temperature 20°C below liquidus reduces erosion depths by a factor of ~2.2. If flow viscosity increases with increasing bubble content in the lava, the presence of 30–50 vol % bubbles leads to erosion depths lower than those relative to bubble-free lava by a factor of ~2.4. The presence of 25 vol % ice in the substrate increases erosion depths by a factor of 1.3. Nevertheless, modeled erosion depths, consistent with the emplacement volume and flow duration constraints, are far less than the depth of the channel (~35–100 m). We conclude that thermal erosion does not appear to have had a major role in excavating Athabasca Valles.

Estimation of small surface displacements in the Upper Rhine Graben area from a combined analysis of PS-InSAR, levelling and GNSS data

Science.gov (United States)

Fuhrmann, T.; Caro Cuenca, M.; Knöpfler, A.; van Leijen, F. J.; Mayer, M.; Westerhaus, M.; Hanssen, R. F.; Heck, B.

2015-10-01

The intra-plate deformation of the Upper Rhine Graben (URG) located in Central Europe is investigated using geodetic measurement techniques. We present a new approach to calculate a combined velocity field from InSAR, levelling and GNSS measurements. As the expected tectonic movements in the URG area are small (less than 1 mm a-1), the best possible solutions for linear velocity rates from single-technique analyses are estimated in a first step. Second, we combine the velocity rates obtained from InSAR (line of sight velocity rates in ascending and descending image geometries), levelling (vertical velocity rates) and GNSS (horizontal velocity rates) using least-squares adjustment (LSA). Focusing on the Northern URG area, we analyse SAR data on four different image stacks (ERS ascending, ERS descending, Envisat ascending, Envisat descending) using the Persistent Scatterer (PS) approach. The linear velocity rates in ascending and descending image geometries, respectively, are estimated in an LSA from joint time-series analysis of ERS and Envisat data. Vertical velocity rates from levelling are obtained from a consistent adjustment of more than 40 000 measured height differences using a kinematic displacement model. Horizontal velocity rates in east and north direction are calculated from a time-series analysis of daily coordinate estimates at 76 permanently operating GNSS sites in the URG region. As the locations, at which the measurement data of PS-InSAR, levelling and GNSS reside, do not coincide, spatial interpolation is needed during several steps of the rigorous processing. We use Ordinary Kriging to interpolate from a given set of data points to the locations of interest with a special focus on the modeling and propagation of errors. The final 3-D velocity field is calculated at a 200 m grid, which carries values only close to the location of PS points, resulting in a mean horizontal and vertical precision of 0.30 and 0.13 mm a-1, respectively. The vertical

Geomorphologic, stratigraphic and sedimentologic evidences of tectonic activity in Sone-Ganga alluvial tract in Middle Ganga Plain, India

Science.gov (United States)

Sahu, Sudarsan; Saha, Dipankar

2014-08-01

The basement of the Ganga basin in the Himalayan foreland is criss-crossed by several faults, dividing the basin into several sub-blocks forming horsts, grabens, or half-grabens. Tectonic perturbations along basement faults have affected the fluvial regime and extent of sediment fill in different parts of the basin during Late Quaternary. The East Patna Fault (EPF) and the West Patna Fault (WPF), located in Sone-Ganga alluvial tract in the southern marginal parts of Middle Ganga Plain (MGP), have remained tectonically active. The EPF particularly has acted significantly and influenced in evolving the geomorphological landscape and the stratigraphic architecture of the area. The block bounded by the two faults has earlier been considered as a single entity, constituting a half-graben. The present investigation (by morpho-stratigraphic and sedimentologic means) has revealed the existence of yet another fault within the half-graben, referred to as Bishunpur-Khagaul Fault (BKF). Many of the long profile morphological characters (e.g., knick-zone, low width-depth ratio) of the Sone River at its lower reaches can be ascribed to local structural deformation along BKF. These basement faults in MGP lie parallel to each other in NE-SW direction.

Del Horizonte Medio al Horizonte Tardío en la Costa Sur Central: el caso del valle de Asia

Directory of Open Access Journals (Sweden)

2004-01-01

Full Text Available DE L’HORIZON MOYEN A L’HORIZON RECENT SUR LA COTE CENTRALE : LE CAS DE LA VALLEE DE ASIA. La vallée de Asia, située à quelque 100 km au sud de Lima, a joué un rôle important durant l’Horizon moyen. En effet, les contextes funéraires de la Huaca Malena et les textiles élaborés qui en sont issus, suggèrent d’étroites relations avec Huari, Pachacamac, et les côtes centrale et nord. L’étude des textiles nous permet de voir que la transition de l’Horizon moyen à la période Intermédiaire récent se marque par une croissance des relations avec la côte centrale. Selon les données ethnohistoriques, la vallée de Asia était durant la période Intermédiaire récent habitée par les Coyallo, qui versaient tribut à Pachacamac. À l’Horizon récent, les Incas construisirent d’importants centres administratifs dans la vallée, et durant cette période le matériel céramique montre de fortes relations avec les styles des vallées voisines au nord, comme Mala, Chilca, et la côte aux alentours de Lima. El valle de Asia, situado a 100 kilómetros al sur de Lima, jugó un rol de importancia durante el Horizonte Medio. En efecto, los contextos funerarios de Huaca Malena, así como los finos textiles que los acompañan indican una fuerte relación con Wari, Pachacamac, la Costa Central y la Costa Norte. De acuerdo con la evidencia textil, el tránsito del Horizonte Medio al periodo Intermedio Tardío incrementó las relaciones con la costa central. Para el periodo Intermedio Tardío, de acuerdo a la información etnohistórica, el valle estuvo habitado por los coayllo, quienes tributaban a Pachacamac. Durante el Horizonte Tardío, los incas construyen importantes centros administrativos en el valle, y la cerámica durante este periodo se relacionó fuertemente con los estilos propios de los vecinos valles norteños de Mala, Chilca y la costa de Lima. FROM THE MIDDLE HORIZON TO THE LATE HORIZON ON THE SOUTH CENTRAL COAST: THE CASE OF THE

Intercambio cationico calcio-magnesio-sodio en algunos suelos del Valle del Cauca

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Torres M. Jorge Ilian

1989-12-01

Full Text Available Para estudiar la influencia de diferentes cantidades de Ca, Mg y Na en las aguas de riego sobre las propiedades químicas y físicas de los suelos, se caracterizó el intercambio Ca-Mg en presencia de diferentes saturaciones de Na en la solución de equilibrio en términos de las isotemas de intercambio de 4 suelos pertenecientes a los tres principales ordenes predominantes en el Valle del Cauca. En general hubo ligera preferencia por Ca sobre Mg en los suelos; pero a bajas concentraciones de Mg en la solución el suelo Doronzoro mostró preferencia por Mg y el suelo Crucero una tendencia hacia mayor afinidad por el Mg+2a altos valores de Mg y de la RAS en la solución. Las preferencias de los suelos por Mg parecen estar asociadas en parte con la presencia de carbonatos y materia orgánica. Con excepción del suelo Crucero, las isotermas no mostraron influencia de la RAS o del PSI resultante sobre la selectividad por Ca+2 o Mg+2. Las altas saturaciones de Mg+2 encontradas en muchos suelos del Valle del Cauca se deben a la presencia de altas cantidades de este ión en las aguas de riego en las aguas freáticas y no a preferencia de los suelos por el mismo.To study the influence of different amounts of Ca, Mg and Na in the irrigation water on chemical and physical properties of soils, four soils from the Cauca Valle y were used to characterize their cation distribution and the Ca-Mg exchange in presence of different concentrations of Na in the equilibrium solution. A general preference for Ca over Mg was found; however, the Doronzoro soil isotherms showed that at low ion concentrations of Mg in the solutions there is a preference for Mg2+relative to Ca2+ and Crucero soil showed an increasing affinity to Mg2+as its concentration and SAR increase in the solution. Soil preferences for magnesium seem to be related to the presence of organic matter or to the presence of carbonates. Excluding the Crucero soil the isotherms did not show influence of SAR

The Nysa-Morava Zone: an active tectonic domain with Late Cenozoic sedimentary grabens in the Western Carpathians' foreland (NE Bohemian Massif)

Czech Academy of Sciences Publication Activity Database

Špaček, P.; Bábek, O.; Štěpančíková, Petra; Švancara, J.; Pazdírková, J.; Sedláček, J.

2015-01-01

Roč. 104, č. 4 (2015), s. 963-990 ISSN 1437-3254 R&D Projects: GA ČR GAP210/12/0573; GA MŠk LM2010008 Institutional support: RVO:67985891 Keywords : Bohemian Massif * Upper Morava Basin * tectonic evolution * seismicity * sedimentary grabens Subject RIV: DB - Geology ; Mineralogy Impact factor: 2.133, year: 2015

Graben Formation and Dike Arrest during the 2009 Harrat Lunayyir Dike Intrusion in Saudi Arabia: Insights from InSAR, Stress Calculations and Analog Experiments

KAUST Repository

Xu, Wenbin; Jonsson, Sigurjon; Corbi, Fabio; Rivalta, Eleonora

2016-01-01

Detailed spatial and temporal accounts of propagating dikes from crustal deformation data, including their interplay with faulting, are rare, leaving many questions about how this interplay affects graben formation and the arrest of dikes unanswered. Here we use InSAR observations, stress calculations and analog experiments to investigate the interaction between an intruding dike and normal faulting during the 2009 Harrat Lunayyir dike intrusion in western Saudi Arabia. We generated five displacement maps from InSAR data to unravel the temporal evolution of deformation covering the majority of the intrusion. We find that the observed surface displacements can be modeled by a ~2-m-thick dike with an upper tip ~2 km below the surface on 16 May 2009, four weeks after the onset of seismic unrest. In the following three days, the dike propagated to within ~1 km of the surface with graben-bounding normal faulting dominating the near-field deformation. The volume of the dike doubled between mid-May and mid-June. We carried out analog experiments that indicate that the wedge-shaped graben grew outwards with the faulting style changing progressively from normal faulting to oblique. Coulomb failure stress change calculations show that the intruding dike caused two zones of shallow horizontal tension on both sides of the dike, producing two zones of fissuring and normal faulting at the surface. In return, the faulting provoked compression around the upper tip of the dike, holding back its vertical propagation.

Graben Formation and Dike Arrest during the 2009 Harrat Lunayyir Dike Intrusion in Saudi Arabia: Insights from InSAR, Stress Calculations and Analog Experiments

KAUST Repository

Xu, Wenbin

2016-03-04

Detailed spatial and temporal accounts of propagating dikes from crustal deformation data, including their interplay with faulting, are rare, leaving many questions about how this interplay affects graben formation and the arrest of dikes unanswered. Here we use InSAR observations, stress calculations and analog experiments to investigate the interaction between an intruding dike and normal faulting during the 2009 Harrat Lunayyir dike intrusion in western Saudi Arabia. We generated five displacement maps from InSAR data to unravel the temporal evolution of deformation covering the majority of the intrusion. We find that the observed surface displacements can be modeled by a ~2-m-thick dike with an upper tip ~2 km below the surface on 16 May 2009, four weeks after the onset of seismic unrest. In the following three days, the dike propagated to within ~1 km of the surface with graben-bounding normal faulting dominating the near-field deformation. The volume of the dike doubled between mid-May and mid-June. We carried out analog experiments that indicate that the wedge-shaped graben grew outwards with the faulting style changing progressively from normal faulting to oblique. Coulomb failure stress change calculations show that the intruding dike caused two zones of shallow horizontal tension on both sides of the dike, producing two zones of fissuring and normal faulting at the surface. In return, the faulting provoked compression around the upper tip of the dike, holding back its vertical propagation.

Las palmeras en los valles principales de la Amazonia peruana

Directory of Open Access Journals (Sweden)

1992-01-01

Full Text Available LES PALMIERS DES PRINCIPALES VALLEES DE L’AMAZONIE PERUVIENNE. La distribution géographique des espèces de palmiers de l’Amazonie péruvienne est présentée selon les principales vallées. Pour chaque affluent important est donnée la liste des espèces récoltées, et pour chaque espèce sont réunies les références des échantillons d’herbiers, collecteur(s et numéro de collection, ainsi que les herbiers de dépôt. Se presenta la distribución de las palmeras de la Amazonia en función de los valles principales. Por cada río de mayor importancia, se da la lista de las especies colectadas, las referencias de las muestras botánicas, colector(es y número de colección, y los herbarios de depósito de dichas muestras. PALMS OF THE MAJOR RIVER VALLEYS OF PERUVIAN AMAZONIA. Palm species distribution in Peruvian Amazonia is presented according to the major river valleys. The species collected are listed for each tributary valley. The collection references, collector(s and number of the specimen and the herbaria of deposit are given for each species.

Genotoxicidad sobre linfocitos humanos expuestos a PM10 de tres sitios del Valle de Aburrá (Antioquia)

OpenAIRE

Mendoza-Zapata, Lady C.; Orozco-Jiménez, Luz Y.; Zapata-Restrepo, Lina M.; Palacio-Baena, Jaime A.

2013-01-01

Objetivo Evaluar la calidad del aire en tres sitios del Valle de Aburrá (Antioquia) a través de la determinación de la genotoxicidad del PM10 en linfocitos humanos. Métodos A partir del valor de referencia de PM10 para Colombia (50 μg/m3/año) se eligieron tres sitios del Valle de Aburrá con diferente promedio de PM10, Barbosa con 25 μg/m3, Corantioquia con 44 μg/m3y Facultad de Minas con 91 μg/m3. Los filtros de PM10 expuestos por 24 horas, se analizaron en la épocas de lluvia, transición y s...

Genotoxicidad sobre linfocitos humanos expuestos a pm10 de tres sitios del valle de aburrá (antioquia)

OpenAIRE

Mendoza, Lady Carolina; Orozco Jimenez, luz Yaneth; Zapata Restrepo, Lina Maria; Palacio Baena, Jaime Alberto

2013-01-01

Objetivo Evaluar la calidad del aire en tres sitios del Valle de Aburrá (Antioquia) a través de la determinación de la genotoxicidad del PM10 en linfocitos humanos.Métodos A partir del valor de referencia de PM10 para Colombia (50 μg/m3/año) se eligieron tres sitios del Valle de Aburrá con diferente promedio de PM10, Barbosa con 25 μg/m3, Corantioquia con 44 μg/m3y Facultad de Minas con 91 μg/m3. Los filtros de PM10 expuestos por 24 horas, se analizaron en la épocas de lluvia, transición y se...

Land degradation trends in upper catchments and morphological developments of braided rivers in drylands: the case of a marginal graben of the Ethiopian Rift Valley

Science.gov (United States)

Demissie, Biadgilgn; Frankl, Amaury; Haile, Mitiku; Nyssen, Jan

2014-05-01

Braided rivers have received relatively little attention in research and development activities in drylands. However, they strongly impact agroecology and agricultural activities and thereby local livelihoods. The Raya Graben (3750 km² including the escarpment) is a marginal graben of the Ethiopian Rift Valley located in North Ethiopia. In order to study the dynamics of braided rivers and the relationship with biophysical controls, 20 representative catchments were selected, ranging between 15 and 311 km². First, the 2005 morphology (length, area) of the braided rivers was related to biophysical controls (vegetation cover, catchment area and slope gradient in the steep upper catchments and gradient in the graben bottom). Second, the changes in length of the braided rivers were related to vegetation cover changes in the upper catchments since 1972. Landsat imagery was used to calculate the Normalized Difference Vegetation Index (NDVI), and to map vegetation cover and the total length of the braided rivers. Spot CNES imagery available from Google Earth was used to identify the total area of the braided rivers in 2005. A linear regression analysis revealed that the length of braided rivers was positively related to the catchment area (R²=0.32, p<0.01), but insignificantly related to vegetation cover in the upper catchments. However, there is an indication that it is an important factor in the relationship calculated for 2005 (R²=0.2, p=0.064). Similarly, the area occupied by the braided rivers was related to NDVI (R²=0.24, p<0.05) and upper catchment area (R²=0.447, p<0.01). Slope gradient is not an important explanatory factor. This is related to the fact that slope gradients are steep (average of 38.1%) in all upper and gentle (average of 3.4%) in graben bottom catchments. The vegetation cover in the upper catchments shows a statistically insignificant increasing trend (R²=0.73, p=0.067) over the last 40 years, whereas length of rivers in the graben bottom

Prevalence of Strongylida nematodes associated with African Snail, Achatina fulica, in Valle del Cauca, Colombia

Directory of Open Access Journals (Sweden)

Diego Córdoba-R

2017-09-01

Full Text Available Objectives. To establish the presence and prevalence of Strongylida nematode parasites in Achatina fulica in the Valle del Cauca, especially of nematodes that are potentially pathogenic for humans. Materials and methods. A. fulica individuals were collected in nine cities of the Valle del Cauca, Colombia. Direct visual examination was used to identify A. fulica parasites. Nematodes were separated from tissue or collected from mucus, washed in saline solution, and fixed in a hot AFA solution. Samples were mounted in glycerine and observed under the microscope. Results. The general nematode parasite prevalence was 35% in 2013. The city with highest prevalence during 2013 was Cartago (60%, following by Buenaventura (42.9% and Cali (33%, while during 2014 were Cali (30% and Buenaventura (30%. The Strongylida nematodes registered were classified in three genera: Angiostrongylus (14.7% prevalence, Aelurostrongylus (2.6%,and Strongyluris (2.6%. The city with highest positive records of Angiostrongylus was Cali during 2014 and Aelurostrongylus was Buenaventura during 2013. Strongyluris genus was recorded only in Cali during 2013, with a prevalence of 11%. Of the nine evaluated cities, five has presence of Angiostrongylus. Conclusions. Three genera of Strongylida nematode were recorded associated with A. fulicas specimens in the Valle del Cauca during 2013 and 2014. Therefore, the role that A. fulica and native mollusk species could be playing in the life cycle of these parasites at the local level should not underestimated.

Relationship between beta lactoglobulin and subclinical mastitis in Valle del Belice sheep breed

NARCIS (Netherlands)

Gigli, I.; Riggio, V.; Monteleone, G.; Cacioppo, D.; Rosa, A.J.M.; Maizon, D.O.

2007-01-01

The objective of the following research was to determine the effect of LGB genotypes on subclinical mastitis in Valle del Belice dairy sheep. Ewes were classified as affected or not by subclinical mastitis within a lactation based on i) a positive culture in one of the test-days and ii) more than

Genetic variability of Harton del Valle by RAM Variabilidad genética de Hartón del Valle mediante RAM

Directory of Open Access Journals (Sweden)

Alvarez Franco Luz Angela

2008-03-01

Full Text Available Harton del Valle (HV breed belong to the seven Creole breeds of the Colombian bovine livestock, according to FAO criteria it is considered as vulnerable. To study its genetical variability, 33 HV animals and three and 3 animals of Holstein breed as a external control were sampled. Simples of DNA were isolated using the Salting Out method and RAM (Random amplified microsatellites technique was used. CGA, CCA, TG and CT primers were used. The mean value of expected heterocigozity was 0.26 and F_ST fue 0.39 ± 0.03. Using Dice–Nei Li index and UPGMA clustering method, two groups were distinguished: the first one integrated for two conservation herds and other one by tour faros that have been sharing breeding bulls.El Hartón del Valle (HV hace parte de las siete razas criollas de ganado bovino colombiano y de acuerdo con los criterios de la FAO está considerado como vulnerable. Para estudiar su variabilidad genética fueron muestreados 33 individuos HV y tres animales de la raza Holstein, como control externo. Se extrajo ADN utilizando el método de Salting Out y las muestras fueron analizadas mediante la técnica molecular RAM (Randon amplified microsatellites. Se utilizaron los cebadores CGA, CCA, TG, y CT. El valor promedio de heterocigosidad esperada fue de 0.26 y el F_ST fue 0.39 ± 0.03. Con el índice de Dice–Nei Li y agrupando con el método UPGMA se distinguieron dos grupos: uno integrado por dos hatos de conservación y el otro por cuatro fincas que han compartido reproductores.

[Detection of Aedes albopictus (Skuse) (Diptera: Culicidae) in the city of Cali, Valle del Cauca, Colombia].

Science.gov (United States)

Cuéllar-Jiménez, María Elena; Velásquez-Escobar, Olga Lucía; González-Obando, Ranulfo; Morales-Reichmann, Carlos Andrés

2007-06-01

Aedes albopictus is the second most important dengue virus vector in the Asian southeast after Aedes aegypti. Its entrance into the Americas occurred in 1985, and laboratory studies performed show its potential as a vector in this continent as well. In Colombia, this species has been reported in Leticia (Amazonas) in 1998 and Buenaventura (Valle del Cauca) in 2001. The latest discoveries show that this mosquito continues to advance toward the country's interior. To inform that the presence of A. albopictus is documented in the city of Cali, Valle del Cauca, Colombia. Since 2002, weekly sampling has been performed using larval traps located at seventeen stations. The identification of the A. albopictus species, was carried out in the Unidad de Entomología, Laboratorio de Salud Pública Departamental. These identifications were confirmed in the Entomology Laboratory at Universidad del Valle and the National Institute of Health in Bogotá. From April to June of 2006, larvae of A. albopictus were found in six sampling stations located between northwest and northeast of Cali, one of them in the suburban area of the Yumbo city. The control of A. aegypti and A. albopictus must be integrated into a single program. The surveillance in the cities and nearest departments must be intensified with the objective of limiting the advancement of A. albopictus.

Neogene and Quaternary geology of a stratigraphic test hole on Horn Island, Mississippi Sound

Science.gov (United States)

Gohn, Gregory S.; Brewster-Wingard, G. Lynn; Cronin, Thomas M.; Edwards, Lucy E.; Gibson, Thomas G.; Rubin, Meyer; Willard, Debra A.

1996-01-01

During April and May, 1991, the U.S. Geological Survey (USGS) drilled a 510-ft-deep, continuously cored, stratigraphic test hole on Horn Island, Mississippi Sound, as part of a field study of the Neogene and Quaternary geology of the Mississippi coastal area. The USGS drilled two new holes at the Horn Island site. The first hole was continuously cored to a depth of 510 ft; coring stopped at this depth due to mechanical problems. To facilitate geophysical logging, an unsampled second hole was drilled to a depth of 519 ft at the same location.

sedimentology, depositional environments and basin evolution

African Journals Online (AJOL)

Preferred Customer

ABSTRACT: The Inter-Trappean coal and oil shale-bearing sedimentation in the Delbi-Moye Basin took place in tectonically controlled grabens and half-grabens formed by extensional fault systems and accompanied by passive subsidence. The sedimentation history of the basin is related to the tectonic events that affected ...

Fluvial terrace formation in the northern Upper Rhine Graben during the last 20 000 years as a result of allogenic controls and autogenic evolution

NARCIS (Netherlands)

Erkens, G.; Dambeck, R.; Volleberg, K.P.; Bouman, M.I.T.J.; Bos, J.A.A.; Cohen, K.M.; Hoek, W.Z.

2009-01-01

The northern Upper Rhine Graben hosts a well-preserved Late Weichselian and Holocene fluvial terrace sequence. Terraces differ in elevation, morphology, and overbank sediment characteristics. The purpose of this study was to determine the relative importance of allogenic controlling factors versus

Magnetostratigraphy of the Dali Basin in Yunnan and implications for late Neogene rotation of the southeast margin of the Tibetan Plateau

NARCIS (Netherlands)

Li, Shihu; Deng, Chenglong; Yao, Haitao; Huang, Sheng; Liu, Chengying; He, Huaiyu; Pan, Yongxin; Zhu, Rixiang

[1] The rotation pattern and fault activity in the southeast margin of the Tibetan Plateau (SEMTP) provide meaningful constraints on the geodynamic evolution of the plateau. However, the lack of Cenozoic paleomagnetic studies and accurate age constraints on Neogene sediments prevents a better

Diagnóstico y propuesta para una gestión integral del riesgo en el valle de aburra: red riesgos

OpenAIRE

ARISTIZÁBAL, EDIER; VARGAS, RICHARD

2010-01-01

A partir del análisis de la situación organizacional de las diferentes instituciones en el Valle de Aburrá frente a la reducción de desastres y emergencias asociadas con los fenómenos de origen natural y antrópico, el Área Metropolitana del Valle de Aburrá, como autoridad ambiental y entidad planificadora, hace una propuesta que pretende articular todas las entidades, organizaciones e instituciones públicas y privadas hacia una gestión integral del riesgo, y la cual denominó: Red para la Gest...

Agroindustrial waste valorization - fruits - in Medellin and the south of Valle de Aburra, Colombia

International Nuclear Information System (INIS)

Yepes, Sandra Milena; Montoya Naranjo, Lina Johana; Orozco Sanchez, Fernando

2008-01-01

Industrial residues continuing being and economic problem so companies have to assume high costs to manage them. Such is the case of large amounts of fruit residues produced in Medellin, city and surroundings due to a great number of companies of this groindustrial sector. In this work a scan was made in Medellin and the South of Valle de Aburra to know the current problem of these residues. Subsequently a physical-chemistry characterization of the most representative residues with the purpose to propose different alternative uses. The main residues of the interviewed companies come from orange, guava, guanabana and mango. The main valorization processes include compost, worms culture and obtaining chemical products. Only with the interviewed companies, plants of waste valorization could be mounted with prosecution capacity from 9 to 375 ton/month depending on process. If all of the residues generated in Medellin and the South of the Valle de Aburra were used, the capacity of these valorization plants could multiply for 20.

Natural radionuclides in the rocks of the Valle del Cervo Pluton in Piedmont.

Science.gov (United States)

Sesana, Lucia; Fumagalli, Marco; Carnevale, Mauro; Polla, Giancarla; Facchini, Ugo; Colombo, Annita; Tunesi, Annalisa; De Capitani, Luisa; Rusconi, Rosella

2006-01-01

Monitoring of the gamma radiation in Valle del Cervo Pluton was performed by determining U and Th contents in the main rock types cropping out over the entire area and pertaining to the granitic complex, syenitic complex and monzonitic complex. In particular, syenitic rocks were largely used as building and ornamental materials (e.g. Sienite della Balma). All the samples are fresh and do not present joints or fractures filled with U minerals. In the crushed samples the activity of uranium varies from 346 to 764 Bq/kg. Concentration of thorium varies from 202 to 478 Bq/kg. For all the analysed rocks uranium activity is higher than thorium one. The lowest value of radioactive concentration is referred to rocks of the granitic complex. The most active rocks are syenites. The data confirm the high activities of Valle del Cervo rock types, strongly connected with high K content of the source magma (geochemical signature); on the contrary, the activity seems to be not related to the location of the samples.

Freshwater gastropods of Neogene and Quaternary lake systems of Europe - state of the art and outlook

Science.gov (United States)

Neubauer, Thomas A.; Harzhauser, Mathias; Mandic, Oleg; Kroh, Andreas

2013-04-01

Globally, about 4000 extant species of freshwater gastropod species have been described. In contrast, only 225 species are listed by MollBase2012 for North- and Central Europe. Many of these are rare species, limited to certain springs and in fact the typical diversity of gastropods in lakes of North and Central Europe is much lower. The high number is boosted by several highly speciose endemic radiations in long-lived ancient lakes, which are hotspots for biodiversity. These long-lived ancient lakes provide key examples for understanding evolutionary processes and therefore are intensively studied. During the Neogene, Europe's geodynamic history gave rise to several such long-lived lakes with conspicuous endemic radiations. However, these lacustrine systems are rare today as well as in the past compared to the enormous numbers of "normal" lakes. Most extant European lakes are mainly results of the Ice Ages and are due to their geologically temporary nature largely confined to the Pleistocene-Holocene. Also deposits of streams, springs, and groundwater, which today are inhabited by species-rich gastropod assemblages, are rarely preserved. Thus, the pre-Quaternary lacustrine record is biased towards long-lived systems. Apart from few general overviews precise studies on the γ-diversities of the post-Oligocene European lake systems and the shifting biodiversity in European freshwater systems through space and time are entirely missing. Even for the modern faunas, literature on large-scale freshwater gastropod diversity in extant lakes is scarce and lacks a statistical approach. Building upon a great amount of existing literature, a new project will provide the first detailed assessment of the composition of European freshwater gastropods during the Neogene and Quaternary at species, genus and family levels, with emphasis on lake faunas. The γ-diversity of several hundred modern and fossil European lakes will be evaluated. Data will be made available permanently for

Estimation of small surface displacements in the Upper Rhine Graben area from a combined analysis of PS-InSAR, levelling and GNSS data

NARCIS (Netherlands)

Fuhrmann, T.; Caro Cuenca, M.; Knöpfler, A.; Leijen, F.J. van; Mayer, M.; Westerhaus, M.; Hanssen, R.F.; Heck, B.

2015-01-01

The intra-plate deformation of the Upper Rhine Graben (URG) located in Central Europe is investigated using geodetic measurement techniques. We present a new approach to calculate a combined velocity field from InSAR, levelling and GNSS measurements. As the expected tectonic movements in the URG

Formation of neogenic ores on the dump-heaps of old uranium mines and on the mine-head of mines under exploitation; Formation de mineraux neogenes sur les haldes d'anciennes mines d'uranium et sur le carreau des mines en exploitation

Energy Technology Data Exchange (ETDEWEB)

Chervet, J [Commissariat a l' Energie Atomique, Saclay (France).Centre d' Etudes Nucleaires

1960-07-01

The aim of this preliminary study is to assess straight away the major degradations suffered by primary and secondary uranium ores under the weathering action of air and water. The uranium ores concerned in this case are those stored in the open air. The pyritic ores are the most vulnerable: the interactions between the pyrite, or rather its oxidation products, and the uraniferous compounds are liable to lead to the formation of neogenic ores, which are of considerable importance in the natural lixiviation of uranium ore stocks. (author) [French] Cette etude preliminaire a pour but de fixer des a present les degradations majeures que subissent les mineraux d'uranium primaires et secondaires, sous l'action de l'air et des eaux meteoriques. Il s'agit en l'occurence des mineraux d'uranium constituant les minerais entreposes a l'air libre. Les minerais pyriteux sont les plus vulnerables: les interactions entre la pyrite ou plutot de ses produits d'oxydation avec les composes uraniferes sont susceptibles de former des mineraux neogenes dont l'importance est considerable dans la lixiviation naturelle des stocks de minerais d'uranium. (auteur)

Neogene shortening and exhumation of the Zagros fold-thrust belt and foreland basin in the Kurdistan region of northern Iraq

Science.gov (United States)

Koshnaw, Renas I.; Horton, Brian K.; Stockli, Daniel F.; Barber, Douglas E.; Tamar-Agha, Mazin Y.; Kendall, Jerome J.

2017-01-01

The Zagros fold-thrust belt in the Kurdistan region of Iraq encroached southward toward a rapidly subsiding Neogene foreland basin and was later partitioned by out-of-sequence shortening focused along the Mountain Front Flexure (MFF), as defined by new low-temperature thermochronologic, stratigraphic, and provenance results. Apatite (U-Th)/He ages document rapid deformation advance from the Main Zagros Fault to southern frontal structures (Kirkuk, Shakal, and Qamar thrusts) at 10-8 Ma, followed by potential basement-involved out-of-sequence development of the MFF (Qaradagh anticline) by 5 Ma. Distinct shifts in detrital zircon U-Pb provenance signatures for Neogene foreland basin fill provide evidence for drainage reorganization during fold-thrust belt advance. U-Pb age spectra and petrologic data from the Injana (Upper Fars) Formation indicate derivation from a variety of Eurasian, Pan-African, ophiolitic and Mesozoic-Cenozoic volcanic terranes, whereas the Mukdadiya (Lower Bakhtiari) and Bai-Hasan (Upper Bakhtiari) Formations show nearly exclusive derivation from the Paleogene Walash-Naopurdan volcanic complex near the Iraq-Iran border. Such a sharp cutoff in Eurasian, Pan-African, and ophiolitic sources is likely associated with drainage reorganization and tectonic development of the geomorphic barrier formed by the MFF. As a result of Zagros crustal shortening, thickening and loading, the Neogene foreland basin developed and accommodated an abrupt influx of fluvial clastic sediment that contains growth stratal evidence of synkinematic accumulation. The apparent out-of-sequence pattern of upper crustal shortening in the hinterland to foreland zone of Iraqi Kurdistan suggests that structural inheritance and the effects of synorogenic erosion and accumulation are important factors influencing the irregular and episodic nature of orogenic growth in the Zagros.

Le graben de l'Anti-Atlas occidental (Maroc) : contrôle tectonique de la paléogéographie et des séquences au Cambrien inférieurThe Lower-Cambrian western Anti-Atlasic graben: tectonic control of palaeogeography and sequential organisation

Science.gov (United States)

Benssaou, Mohammed; Hamoumi, Naı̈ma

2003-03-01

In the Moroccan western Anti-Atlas, the combined extensive tectonic events with a long-term sea-level rise is the main factor on building vertical stacking transgressive-regressive sequences. In the Ait Abdallah-Boussafene axis, the subsidence processes, relayed by a brutal platform tilting generated an elongated NE-SW graben. This is an evidence of the persistence of the Anti-Atlasic rifting process during the last part of the Lower-Cambrian succession.

The Valles natural analogue project

International Nuclear Information System (INIS)

Stockman, H.; Krumhansl, J.; Ho, C.; McConnell, V.

1994-12-01

The contact between an obsidian flow and a steep-walled tuff canyon was examined as an analogue for a highlevel waste repository. The analogue site is located in the Valles Caldera in New Mexico, where a massive obsidian flow filled a paleocanyon in the Battleship Rock tuff. The obsidian flow provided a heat source, analogous to waste panels or an igneous intrusion in a repository, and caused evaporation and migration of water. The tuff and obsidian samples were analyzed for major and trace elements and mineralogy by INAA, XRF, X-ray diffraction; and scanning electron microscopy and electron microprobe. Samples were also analyzed for D/H and 39 Ar/ 4O isotopic composition. Overall,the effects of the heating event seem to have been slight and limited to the tuff nearest the contact. There is some evidence of devitrification and migration of volatiles in the tuff within 10 meters of the contact, but variations in major and trace element chemistry are small and difficult to distinguish from the natural (pre-heating) variability of the rocks

Distribución espacial del Bosque Seco Tropical en el Valle del Cauca, Colombia

Directory of Open Access Journals (Sweden)

Diana Patricia Alvarado-Solano

2015-09-01

Full Text Available En el departamento del Valle del Cauca, la distribución de Bosque Seco Tropical (BsT se ha asociado al valle geográfico del río Cauca ubicado en la zona plana. Actualmente en esta zona, su cobertura se ha reducido a pocos relictos que se encuentran bajo alguna figura de conservación y mantienen áreas representativas de las formaciones vegetales sssstípicas de este bioma. Este trabajo se enfocó en el reconocimiento de la distribución espacial de formaciones vegetales de BsT en el departamento del Valle del Cauca. Se empleó información cartográfica secundaria para reconocer los biomas, ecosistemas y usos del suelo del área de estudio y en zonas adyacentes del piedemonte y montañas. Un modelo digital de elevaciones fue utilizado para realizar análisis altitudinales. En un sistema de información geográfico se aplicaron técnicas de geoprocesamiento y análisis geoespacial entre la información cartográfica y satelital. Los resultados evidencian que pese al avanzado deterioro de las coberturas de bosque seco en la zona plana, alrededor del 80 % se localiza en ecosistemas de montaña, específicamente en zonas de transición hacia bosques húmedos. A futuro, el potencial de estas áreas deberá evaluarse para ser incluidas en estrategias de conservación y restauración del bosque seco así como en el diseño de procesos adaptativos frente al cambio climático.

Rethinking CCD's Significance in Estimating Late Neogene Whole Ocean Carbonate Budget

Science.gov (United States)

Si, W.; Rosenthal, Y.

2017-12-01

The global averaged calcite compensation depth (CCD) record is conventionally used to reconstruct two correlatable parameters of the carbonate system - the alkalinity budget of the ocean and/or the saturation state of the ocean. Accordingly, the available CCD reconstructions have been interpreted to suggest either relative stable (Pearson and Palmer, 2000) or increased alkalinity of the ocean over the past 15 Ma (Tyrrell and Zeebe, 2004; Pälike et al., 2012). However, CCD alone is insufficient to constrain the carbonate system because the weathering flux of alkalinity into the ocean is not only balanced by CaCO3 dissolution on the seafloor but also by the biologic production in the euphotic zone and, the CCD records cannot be readily interpreted as changes in either process. Here, we present evidence of the co-evolution of surface CaCO3 production and deepsea dissolution through the late Neogene. By examining separately the mass accumulation rates (MAR) of coccoliths, planktonic foraminifera, and quantifying dissolution (using a proxy revised from Broecker et al., 1999) in seventeen deepsea cores from multiple depth-transects, we find that 1) MAR of dissolution-resistant coccoliths was substantially higher in the mid Miocene and declining on a global scale towards the present; 2) unlike coccoliths, MAR of planktonic foraminifera, shows no apparent secular trend through that time; 3) the revised dissolution index, shows significantly improved preservation of planktonic foraminiferal shells over that time, particularly at intermediate water depth and exhibits close association between changes in preservation with key climatic events. Our new records have two immediate implications. First, the substantially weakened pelagic biogenic carbonate production from mid Miocene to present alone could account for the improved preservation of deepsea carbonates without calling for a scenario of increased weathering input. Second, with the constrain of global averaged CCD

The Neogene Environment of the Beardmore Glacier, Transantarctic Mountains

Science.gov (United States)

Ashworth, A. C.; Cantrill, D. J.; Francis, J. E.; Roof, S. R.

2004-12-01

Discontinuous sequences of Neogene marine and non-marine glacigenic sequences, including the Meyer Desert Formation (MDF), occur throughout the Transantarctic Mountains. The upper 85m of the MDF, consisting of interbedded diamictites, conglomerates, sandstones and siltstones, outcrops in the Oliver Bluffs on the Beardmore Glacier at 85° 07'S, 166° 35'E. The location is about 170 km south of the confluence of the Beardmore Glacier with the Ross Ice Shelf and about 500 km north of the South Pole The glacial, fluvioglacial and glaciolacustrine facies of the MDF represent a dynamic glacial margin which advanced and retreated on at least four occasions. On at least one occasion, the retreat was sufficiently long for plants and animals to colonize the head of a major fjord which existed in the place of the existing Beardmore Glacier. From the fossils we have identified at least 18 species of plants, 3 species of insects, 2 species of freshwater mollusks, and a species of fish. The plant fossils consist of pollen, seeds, fruits, flowers, leaves, wood, and in situ plants. The plants include a cryptogamic flora of mosses and liverworts, conifers, and angiosperms in the families Gramineae, Cyperaceae, Nothofagaceae, Ranunculaceae, Hippuridaceae, ?Caryophyllaceae, and ?Chenopodiaceae or ?Myrtaceae. The plants grew in a weakly developed soil developed on a complex periglacial environment that included moraines, glacial outwash streams, well-drained gravel ridges, and poorly drained depressions in which peat and marl were being deposited. The fossil assemblage represents a mosaic tundra environment of well- and poorly-drained micro-sites, in which nutrient availability would have been patchily distributed. Antarctica has been essentially in a polar position since the Early Cretaceous and at 85° S receives no sunlight from the middle of March until the end of September. Today, the annual radiation received is about 42% that of Tierra del Fuego at 55° S. During the Neogene

FAUNA ANFIBIA DEL VALLE DE SIBUNDOY, PUTUMAYO-COLOMBIA

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MUESES-CISNEROS JONH JAIRO

2005-12-01

Full Text Available La fauna Amphibia del Valle de Sibundoy consta de 32 especies agrupadas en dos órdenes, cinco familias y siete géneros. De éstas, cinco son especies nuevas cuya descripción se encuentra en proceso. Se amplía el límite altitudinal de otras siete y se presentan tres más para ser incluidas en la lista de anfibios de Colombia. A pesar de que en el lugar se han realizado colectas herpetológicas desde finales de los años sesenta, este estudio es el primero que se realiza en el Putumayo (uno de los departamentos menos muestreados del país.

Paleointensity Variation of The Earth's Magnetic Field Obtained from Neogene and Quaternary Volcanic Rocks in Central Anatolian Plateau

Science.gov (United States)

Kaya, Nurcan; Makaroǧlu, Özlem; Hisarlı, Z. Mümtaz

2017-04-01

We present the variation of the earth magnetic field intensity obtained from Neogene and Quaternary volcanic rocks located in the Central Anatolian plateau. Total of four hundred and fifty volcanic rocks were sub-sampled in eighteen different sites around the study region. A modified Thellier method including the Leonhardt protocol was used to determine paleointensity values. Paleointensity results from ten sites were accepted according to the confidence criteria . According to first results the average total paleointensity field values, indicated by F, are 51.797±5.044 μT for site NK8,NK17,NK18,NK15 with age of 4.4-10.7 my, 51.91±4.651 for site NK4, NK3, NK12, NK6, NK11, NK14 with age of 0.1-2.6 m.y. The average VDMs (Virtual Dipol Moments) correspond to 8.39x1022 , 8.92x1022 Am2 for the four Neogene and six Quaternary rocks sites respectively. Our data were correlated with IAGA database that were obtained from the surrounding area. The correlation showed that the paleointensity data from the Central Anatolia plateau considerably agree with the IAGA data.

The Half-Half Plot

NARCIS (Netherlands)

Einmahl, J.H.J.; Gantner, M.

2009-01-01

The Half-Half (HH) plot is a new graphical method to investigate qualitatively the shape of a regression curve. The empirical HH-plot counts observations in the lower and upper quarter of a strip that moves horizontally over the scatter plot. The plot displays jumps clearly and reveals further

The half-half plot

NARCIS (Netherlands)

Einmahl, J.H.J.; Gantner, M.

2012-01-01

The Half-Half (HH) plot is a new graphical method to investigate qualitatively the shape of a regression curve. The empirical HH-plot counts observations in the lower and upper quarter of a strip that moves horizontally over the scatterplot. The plot displays jumps clearly and reveals further

Epidemiologia del parasitismo intestinal infantil en el Valle del Guadalquivir

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Pérez Armengol Cristina

1997-01-01

Full Text Available FUNDAMENTO: Las parasitosis intestinales en los niños constituyen un problema de salud pública que debe ser valorado periódicamente en cada región. En este trabajo se aborda, por primera vez en la región natural del Valle del Guadalquivir, un estudio amplio sobre la prevalencia del parasitismo intestinal en la población infantil de la zona. MÉTODOS: Durante el período 1994-1996, mediante análisis coprológico y método de Graham, se ha estudiado a 1.917 niños y niñas asintomáticos, con edades comprendidas entre seis y diez años, residentes en veinte localidades del Valle del Guadalquivir. RESULTADOS: El índice global de parasitación ha sido del 27,12 %. Las especies parásitas detectadas, así como sus prevalencias fueron: Enterobius vermicularis (20,44%, Giardia lamblia (5,05%, Entamoeba coli (2,45%, Endolimax nana (1,61%, Entamoeba histolytica (0,31%, Entamoeba hartmanni (0,05%, Iodamoeba bütschlii (0,05%. CONCLUSIONES: La prevalencia global encontrada es similar a la de otras regiones españolas, aunque quizás pueda considerarse algo más favorable. No se detectan geohelmintos, debido posiblemente a la mejora de la infraestructura higiénico-sanitaria y a los efectos de la prolongada sequía en la zona. La giardiasis, a diferencia de las restantes protozoosis, mantiene una prevalencia relativamente alta.

Levels of Heavy Metals in Adolescents Living in the Industrialised Area of Milazzo-Valle del Mela (Northern Sicily

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Monica Interdonato

2014-01-01

Full Text Available In the Milazzo-Valle del Mela area, the presence of industrial plants and the oil refinery make local residents concerned for their health. For this reason, we evaluated the levels of heavy metals in 226 children aged 12–14 years, living in the 7 municipalities of the area. A control age-matched population (n=29 living 45 km far from the industrial site was also enrolled. Arsenic, cadmium, chromium, mercury, nickel, and vanadium were analysed in 24 h urine samples, while lead concentration was evaluated in blood samples. A questionnaire regarding life style and risk perception was also administered. Adolescents from Milazzo-Valle del Mela had cadmium levels significantly higher compared to either controls  (P<0.0001 or the reference values of the European Germany Environmental Survey (GerES-IV and the American National Health and Nutrition Examination Survey (NHANES. Furthermore, children had higher perception of living in a high-risk environment. The present data, for the first time, clearly indicate that adolescents living in Milazzo-Valle del Mela have increased body concentration of cadmium, which may be harmful to human health. These results deserve particular attention by the local and regional government to initiate prevention programmes in this susceptible population.

Overview of naturally permeable fractured reservoirs in the central and southern Upper Rhine Graben: Insights from geothermal wells

OpenAIRE

Vidal , Jeanne; Genter , Albert

2018-01-01

International audience; Since the 1980′s, more than 15 geothermal wells have been drilled in the Upper Rhine Graben (URG), representing more than 60 km of drill length. Although some early concepts were related to purely matrix-porosity reservoirs or Hot Dry Rock systems, most projects in the URG are currently exploiting the geothermal resources that are trapped in fracture networks at the base of the sedimentary cover and in the granitic basement. Lessons-learnt from the European EGS referen...

Diagnóstico y propuesta para una gestión integral del riesgo en el Valle de Aburrá: red riesgos.

OpenAIRE

Aristizábal, Edier; Vargas, Richard; Mesa Sánchez, Óscar José

2008-01-01

A partir del análisis de la situación organizacional de las diferentes instituciones en el Valle de Aburrá frente a la reducción de desastres y emergencias asociadas con los fenómenos de origen natural y antrópico, el Área Metropolitana del Valle de Aburrá, como autoridad ambiental y entidad planificadora, hace una propuesta que pretende articular todas las entidades, organizaciones e instituciones públicas y privadas hacia una gestión integral del riesgo, y la cual denominó: Red para la Gest...

Petrology and provenance of the Neogene fluvial succession in Pishin Belt (Katawaz Basin) western Pakistan: Implications for sedimentation in peripheral forelands basins

DEFF Research Database (Denmark)

Kasi, Aimal Khan; Kassi, Aktar Muhammad; Friis, Henrik

2017-01-01

Sandstones and conglomerates of the Neogene fluvial succession in Pishin Belt (Katawaz Basin), Pakistan were studied for the first time to understand the composition, provenance and tectonic settings of the source areas. Sandstones of the Miocene Dasht Murgha Group and Pliocene Malthanai Formatio...

Preliminary characterization of the Green Antioquian consumer: the case of the consumers from Valle de Aburra

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Nelcy Rocío Escobar Moreno

2015-07-01

Full Text Available Rev.esc.adm.neg This research paper aims at identifying the profile of green consumers living in Valle de Aburra, in Antioquia, to identify the specific features and needs of this group as a market segment. At first, this article shows a conceptual framework about terms such as green market, green consumers and green products. Then, a research methodology is described based on a quantitative formulation of a piloting study, through which a measurement instrument having 14 questions divided into different variables product, price, distribution and communication collected key information to get to preliminary conclusions about consumers as its main object of study. Finally, a statistic descriptive analysis was made to get the profile of green consumers living in Valle de Aburra and a proposal describing key elements to set the bases for future investigations about this topic.

Chapter 9. The Valles Caldera National Preserve as a multi-layered ethnographic landscape

Science.gov (United States)

Kurt F. Anschuetz

2007-01-01

The land use history of the Valles Caldera National Preserve (VCNP), as represented in the documentary record maintained in various archives and libraries, focuses primarily on the Hispanic and Anglo-American occupation of the locale subsequent to 1860. In an act of June 21, 1860, the U.S. Congress authorized the Baca Land Grant heirs to choose as many as five square...

Metamorphic history of the Central Pyrenees Part II, Valle de Arán, Sheet 4

NARCIS (Netherlands)

Zwart, H.J.

1963-01-01

The structural geology and metamorphic petrology of the Bosost area in the Valle de Arán (Central Pyrenees) is discussed. The rocks exposed in this area consist of Cambro-Ordovician mica-schists with numerous granite and pegmatite bodies, phyllites and limestones; Silurian slates and schists and

A reevaluation of the lineage development of Pararotalia and Praepararotalia including new material from the Rupelian of the southern Upper Rhine Graben

Science.gov (United States)

Pirkenseer, C.; Spezzaferri, S.

2009-04-01

The lineage of the benthic Foraminifera Praepararotalia and Pararotalia has a known record since the Late Cretaceous to recent. Showing a wide range of morphologic variations, the most recent thorough generic definition of Pararotalia is heavily based on internal structures (e.g., HOTTINGER et al. 1991). Thus many of the older, not revised species are still assigned to Pararotalia by means of visible external structures. This applies also to the genus Praepararotalia (Cretaceous to Late Eocene), erected by LIU et al. (1998) as a "simple" predecessor-taxon with generally round, smooth to pustulated chambers of slowly increasing diameter, very low to flat spiral side and small overall size. Wall texture and aperture are identical in both genera. According to LIU et al. (1998) Pararotalia s.str. is characterized by a general size increase, planoconvex test, the development of peripheral pseudospines, keel and increasingly conical chambers ("angular" habitus) as well as a distinct umbilical sutures and plug. Pararotalia macneilli (Danian) and P. ishamae (Thanetian) are considered to represent linking species, the main difference being the initial development of an umbilical plug. The separation of the two genera took place in the Late Cretaceous or Earliest Paleogene, with Praepararotalia cretacea being the ancestral species (LIU et al. 1998). We present here a reevaluation of the morphogroups based on material from the Rupelian of the southern Upper Rhine Graben and the analysis of the record of reported species from literature. Four different groups can be separated in terms of external morphology. The first group represents the Praepararotalia-habitus of small size. New material from the Rupelian of the southern Upper Rhine Graben may be attributed to this group. It differs in a higher number of chambers in the last whorl and total chamber numbers (5-6 vs. 6-7, 11-16 vs. up to 22), a much larger size (up to 500µm) and a higher trochospire. Some specimens show a

Stratigraphy of Neogene deposits in the Khania province, Crete, with special reference to foraminifera of the family Planorbulinidae and the genus Heterostegina

NARCIS (Netherlands)

Freudenthal, T.

1969-01-01

In this paper the stratigraphy of the Neogene deposits in the Khania Province, Crete, Greece, is described. Special attention is paid to the evolution and taxonomy of foraminiferal genera assigned previously to the family Planorbulinidae. This partial revision of the Planorbulinidae is based not

The stratigraphy and regional structure of Miocene deposits in western Amazonia (Peru, Colombia and Brazil), with implications for late Neogene landscape evolution

NARCIS (Netherlands)

Wesselingh, F.P.; Hoorn, M.C.; Guerrero, J.; Räsänen, M.E.; Romero Pittmann, L.; Salo, J.A.

2006-01-01

A biozonation based on molluscs is proposed for Miocene deposits of western Amazonia (Peru, Colombia and Brazil), commonly referred to as the Pebas Formation. The new zonation refines existing pollen zonations and provides a key for the quick assessment of the stratigraphic position of Neogene

Time-to-event analysis of mastitis at first-lactation in Valle del Belice ewes

NARCIS (Netherlands)

Portolano, B.; Firlocchiaro, R.; Kaam, van J.B.C.H.M.; Riggio, V.; Maizon, D.O.

2007-01-01

A time-to-event study for mastitis at first-lactation in Valle del Belice ewes was conducted, using survival analysis with an animal model. The goals were to evaluate the effect of lambing season and level of milk production on the time from lambing to the day when a ewe experienced a test-day with

VALORIZACIÓN DE RESIDUOS AGROINDUSTRIALES - FRUTAS - EN MEDELLÍN Y EL SUR DEL VALLE DEL ABURRÁ, COLOMBIA AGROINDUSTRIAL WASTE VALORIZATION - FRUITS - IN MEDELLÍN AND THE SOUTH OF VALLE DE ABURRÁ, COLOMBIA

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Sandra Milena Yepes

2008-06-01

Full Text Available Los residuos industriales siguen convirtiéndose en un gran problema no sólo ambiental sino económico, ya que las mismas empresas tienen que asumir altos costos de disposición de éstos. Tal es el caso de la gran cantidad de residuos de frutas que se producen en la ciudad de Medellín y sus alrededores, debido al número extenso de empresas de este sector agroindustrial. En el presente trabajo se realizó un sondeo en Medellín y el Sur del Valle del Aburrá para conocer la problemática actual de estos residuos. Posteriormente se realizó una caracterización físico-química a los residuos más representativos que permitiera proponer diferentes alternativas de aprovechamiento. Los principales residuos de las empresas encuestadas provienen de naranja, guayaba, guanábana y mango. Los principales procesos de valorización incluyen el compostaje, la lombricultura y la obtención de productos químicos. Sólo con las empresas encuestadas podrían montarse plantas de valorización de residuos con capacidad de procesamiento de 9 a 375 ton/mes, dependiendo del proceso. Si se utilizaran todos los residuos generados en Medellín y el Sur del Valle del Aburrá, la capacidad de estas plantas de valorización podrían multiplicarse por 20.Industrial residues continuing being and economic problem so companies have to assume high costs to manage them. Such is the case of large amounts of fruit residues produced in Medellín, city and surroundings due to a great number of companies of this agroindustrial sector. In this work a scan was made in Medellín and the South of Valle de Aburrá to know the current problem of these residues. Subsequently a physical-chemistry characterization of the most representative residues with the purpose to propose different alternative uses. The main residues of the interviewed companies come from orange, guava, guanabana and mango. The main valorization processes include compost, worms culture and obtaining chemical

Biodiversity and paleobiogeography of the European freshwater Neogene: trends, hotspots and faunal turnovers

Science.gov (United States)

Neubauer, Thomas A.; Harzhauser, Mathias; Georgopoulou, Elisavet; Andreas, Kroh; Mandic, Oleg

2015-04-01

We present an outline of a paleobiogeographic framework for the European fresh- and brackish-water systems during the Neogene. Data basis is a presence-absence matrix of lacustrine gastropods from over 2,700 localities. Cluster analyses were separately carried out on the datasets of the four time slices Early Miocene, Middle Miocene, Late Miocene, and Pliocene. Based on the results of the cluster analyses, the degree of endemicity, and geographical coherence, we classified the lake systems of the four time intervals into biogeographic units. The increasing degree of provincialism throughout the Neogene supported more detailed breakdowns in younger intervals. This pattern reflects the ongoing continentalization of Europe linked to the Alpidic Orogenesis. Additionally, the retreat of the Paratethys Sea and its isolation from the Mediterranean promoted the evolution of endemic faunas in surrounding lacustrine systems. Direct descendants such as long-lived Lake Pannon, Lake Dacia or Lake Slavonia persisted over several millions of years and promoted the evolution of highly diverse and endemic faunas. Because of their extensive duration they crucially influenced family-level composition, differences of the relative species richnesses per biogeographic unit, and rising rate of endemicity. We show that the biogeographic classification as well as the existence of biodiversity hotspots are tightly linked to the formation and evolution of long-lived lacustrine environments and thus to Europe's geodynamic history. Heat maps are provided to visualize the shifting distributions of hotspots through time. The only physiographic factor that can be shown to be correlated with species richness is the size of a lake. Other factors such as latitude, longitude or temporal duration show weak relationships. Correlation of biodiversity trends to climatic parameters such as temperature and precipitation are feasible only for selected periods. Climate is considered to have only minor

Tectono-sedimentary events and geodynamic evolution of the Mesozoic and Cenozoic basins of the Alpine Margin, Gulf of Tunis, north-eastern Tunisia offshore

Science.gov (United States)

Melki, Fetheddine; Zouaghi, Taher; Chelbi, Mohamed Ben; Bédir, Mourad; Zargouni, Fouad

2010-09-01

The structural pattern, tectono-sedimentary framework and geodynamic evolution for Mesozoic and Cenozoic deep structures of the Gulf of Tunis (north-eastern Tunisia) are proposed using petroleum well data and a 2-D seismic interpretation. The structural system of the study area is marked by two sets of faults that control the Mesozoic subsidence and inversions during the Paleogene and Neogene times: (i) a NE-SW striking set associated with folds and faults, which have a reverse component; and (ii) a NW-SE striking set active during the Tertiary extension episodes and delineating grabens and subsiding synclines. In order to better characterize the tectono-sedimentary evolution of the Gulf of Tunis structures, seismic data interpretations are compared to stratigraphic and structural data from wells and neighbouring outcrops. The Atlas and external Tell belonged to the southernmost Tethyan margin record a geodynamic evolution including: (i) rifting periods of subsidence and Tethyan oceanic accretions from Triassic until Early Cretaceous: we recognized high subsiding zones (Raja and Carthage domains), less subsiding zones (Gamart domain) and a completely emerged area (Raouad domain); (ii) compressive events during the Cenozoic with relaxation periods of the Oligocene-Aquitanian and Messinian-Early Pliocene. The NW-SE Late Eocene and Tortonian compressive events caused local inversions with sealed and eroded folded structures. During Middle to Late Miocene and Early Pliocene, we have identified depocentre structures corresponding to half-grabens and synclines in the Carthage and Karkouane domains. The north-south contractional events at the end of Early Pliocene and Late Pliocene periods are associated with significant inversion of subsidence and synsedimentary folded structures. Structuring and major tectonic events, recognized in the Gulf of Tunis, are linked to the common geodynamic evolution of the north African and western Mediterranean basins.

Gravity and magnetic survey of the Oaxaca city region: Cenozoic horst-and-graben structure superimposed on the Oaxaca-Juarez terrane boundary, southern Mexico

Science.gov (United States)

Campos-Enríquez, J. O.; Belmonte-Jiménez, S. I.; Keppie, J. D.; Ortega-Gutiérrez, F.; Arzate, J. A.; Martínez-Silva, J.; Martínez-Serrano, R. G.

2010-04-01

A geophysical survey of the Oaxaca Fault along the north-trending Etla and Zaachila valleys area, southern Mexico, shows a series of NNW-SSE Bouguer and magnetic anomalies with steeper gradients towards the east. The Oaxaca Fault represents Tertiary extensional reactivation of the Juarez shear zone that constitutes the boundary between the Oaxaca and Juárez terranes. Cooperative interpretation of six combined gravity and magnetic NE-SW profiles perpendicular to the valleys indicates the presence of a composite depression comprising three N-S sub-basins: the northern Etla and southern Zaachila sub-basins separated by the Atzompa sub-basin. The Etla sub-basin is bounded by the moderately E-dipping, Etla Fault and the more steeply W-dipping Oaxaca Fault, which together constitute a graben that continues southwards into the Atzompa graben. The deeper Zaachila sub-basin, south of Oaxaca city, is a wide V-shaped graben with a horst in the middle. The new geophysical data suggest that the Oaxaca-Juarez terrane boundary is displaced sinistrally ca. 20 km along the E-W Donají Fault, which defines the northern boundary of the Zaachila sub-basin. On the other hand, the Oaxaca Fault may either continue unbroken southwards along the western margin of the horst in the Zaachila sub-basin or be offset along with the terrane boundary. The sinistral movement may have taken place either during the Late Mesozoic-Early Cenozoic, Laramide Orogeny as a lateral ramp in the thrust plane or under Miocene-Pliocene, NE-SW extension. The former suggests that the Donají Fault is a transcurrent fault, whereas the latter implies that it is a transfer fault. The models imply that originally the suture was continuous south of the Donaji Fault and provide a constraint for the accretion of the Oaxaca and Juarez terranes.

Données récentes de l'épidémiologie de la fièvre de la Vallée du Rift (F.V.R.) au Sénégal

OpenAIRE

Thiongane, Y.; Thonnon, J.; Zeller, H.; Lo, M. M.; Faty, A.; Diagne, F.; Gonzalez, J.; Akakpo, J. A.; Fontenille, Didier; Digoutte, J. P.

1998-01-01

La fièvre de la Vallée du Rift est une anthropozoonose largement répandue en Afrique. En 1987, s'est déclarée une épidémie très meurtrière de la fièvre de la Vallée du Rift (FVR) dans la Basse Vallée du Fleuve Sénégal. En raison du risque de réactivation, un programme de surveillance sérologique a été mis en place dans des zones sahéliennes cibles : vallées du Sénégal et Ferlo. Des troupeaux de ruminants domestiques (bovins, ovins et caprins) ont été régulièrement surveillés et testés. Les sé...

Primer registro de Phyllodactylus sentosus (Squamata: Phyllodactylidae) para el valle del río Chillón, Lima, Perú

OpenAIRE

Diego Olivera; Luis Castillo; Gerardo Gutiérrez

2016-01-01

El gecko de Lima Phyllodactylus sentosus (Dixon & Huey, 1970) identificado como en peligro crítico de extinción ha sido registrado sólo en algunas localidades entre los valles de los ríos Rímac y Lurín, en el centro y sur de la ciudad de Lima, Región Lima, sin embargo, su distribución hacia el norte no está documentada. En el presente trabajo se reporta por primera vez la presencia de P. sentosus en la Huaca Tambo Inga, ubicada en el margen derecho del valle del río Chillón en el distrito de ...

Application of low-enthalpy geothermal energy in the New Hospital of Mollet del Valles; Aplicacion de la geotermia de baja entalpia en el nuevo Hospital de Mollet del Valles

Energy Technology Data Exchange (ETDEWEB)

Cuesta Garcia, M. A.; Mayoral Fernandez, G. R.

2009-07-01

The new Hospital in the city of Mollet del Valles has chosen Geothermic energy for heating and cooling. The installation, built between year 2007 to 2009, will turn the hospital into one of the most sustainable building of Spain because will supply more than 1 MW of heating and cooling peak load with Goethermic energy. Now, this project is the biggest in Spain and it is one of the five biggest in all Europe. (Author)

La Pachahuara de Acolla: una danza de los esclavos negros en el valle de Yanamarca

Directory of Open Access Journals (Sweden)

1976-01-01

Full Text Available La danse 'Pachahuara' se pratique pendant la Noël dans la vallée du rio Mantaro (Pérou central et son origine remonte à l'arrivée d'esclaves noirs dans la sierra péruvienne (Jauja, 1533. La danse décrite est celle de la communauté d'Acolla (N de Huancayo}. Une description des costumes des différents personnages est donnée avant de passer à la chorégraphie proprement dite. Deux phases caractérisent le pachahuara, avec une musique bien différenciée. Une tentative d'interprétation suit la description, s'appuyant sur des données historiques concernant l'établissement d'esclaves noirs dans la vallée du Mantaro la danse symboliserait l'esclavitude puis la liberté retrouvée. El baile 'Pachahuara' se practica durante la Navidad en el valle del río Mantaro (Perú Central y su origen se remonta a la llegada de esclavos negros en la sierra peruana (Jauja, 1533. La danza descrita es la de la comunidad de Acolla (N de Huancayo. Una descripción de los trajes de los distintos personajes ha sido dada antes de pasar a la coreografía propiamente dicha. Dos fases caracterizan la pachahuara, con una música bien diferenciada. Una tentativa de interpretación sigue a la descripción, basándose en datos históricos referentes al establecimiento de esclavos negros en el valle del Mantaro la danza simbolizaría la esclavitud y después la libertad recuperada. The dance 'Pachahuara' is practiced during the Christmas times in the valley of the Rio Mantaro (Central Peru and its origin dates back to the coming of the black slaves in the peruvian sierra (Jauja, 1533. The dance described is that of the Acolla community (North of Huancayo. A description of the different personnages'clothes is given before analyzing the choreography itself. Two phases characterize the pachahuara, with a well differenced music. An attempt of interpretation is following the description, basing it upon historical referring concerning the establishment of the black slaves

Evolution of the soil humus status on the calcareous Neogene clay dumps of the Sokolov quarry complex in the Czech Republic

Czech Academy of Sciences Publication Activity Database

Abakumov, E.V.; Frouz, Jan

2009-01-01

Roč. 42, č. 7 (2009), s. 718-724 ISSN 1064-2293 Grant - others:Russian Foundation for Basic Research(XE) 08-04-01128 Institutional research plan: CEZ:AV0Z60660521 Keywords : soil humus status * calcareous Neogene clay dumps * Sokolov quarry complex Subject RIV: EH - Ecology, Behaviour Impact factor: 0.222, year: 2009

Recent surface displacements in the Upper Rhine Graben — Preliminary results from geodetic networks

Science.gov (United States)

Fuhrmann, Thomas; Heck, Bernhard; Knöpfler, Andreas; Masson, Frédéric; Mayer, Michael; Ulrich, Patrice; Westerhaus, Malte; Zippelt, Karl

2013-08-01

Datasets of the GNSS Upper Rhine Graben Network (GURN) and the national levelling networks in Germany, France and Switzerland are investigated with respect to current surface displacements in the Upper Rhine Graben (URG) area. GURN consists of about 80 permanent GNSS (Global Navigation Satellite Systems) stations. The terrestrial levelling network comprises 1st and 2nd order levelling lines that have been remeasured at intervals of roughly 25 years, starting in 1922. Compared to earlier studies national institutions and private companies made available raw data, allowing for consistent solutions for the URG region. We focussed on the southern and eastern parts of the investigation area. Our preliminary results show that the levelling and GNSS datasets are sensitive to resolve small surface displacement rates down to an order of magnitude of 0.2 mm/a and 0.4 mm/a, respectively. The observed horizontal velocity components for a test region south of Strasbourg, obtained from GNSS coordinate time series, vary around 0.5 mm/a. The results are in general agreement with interseismic strain built-up in a sinistral strike-slip regime. Since the accuracy of the GNSS derived vertical component is insufficient, data of precise levelling networks is used to determine vertical displacement rates. More than 75% of the vertical rates obtained from a kinematic adjustment of 1st order levelling lines in the eastern part of URG vary between - 0.2 mm/a and + 0.2 mm/a, indicating that this region behaves stable. Higher rates up to 0.5 mm/a in a limited region south of Freiburg are in general agreement with active faulting. We conclude that both networks deliver stable results that reflect real surface movements in the URG area. We note, however, that geodetically observed surface displacements generally result from a superposition of different effects, and that a separation in tectonic and non-tectonic processes needs additional information and expertise.

Historical coseismic surface deformation of fluvial gravel deposits, Schafberg fault, Lower Rhine Graben, Germany

Science.gov (United States)

Kübler, Simon; Friedrich, Anke M.; Gold, Ryan D.; Strecker, Manfred R.

2018-03-01

Intraplate earthquakes pose a significant seismic hazard in densely populated rift systems like the Lower Rhine Graben in Central Europe. While the locations of most faults in this region are well known, constraints on their seismogenic potential and earthquake recurrence are limited. In particular, the Holocene deformation history of active faults remains enigmatic. In an exposure excavated across the Schafberg fault in the southwestern Lower Rhine Graben, south of Untermaubach, in the epicentral region of the 1756 Düren earthquake ( M L 6.2), we mapped a complex deformation zone in Holocene fluvial sediments. We document evidence for at least one paleoearthquake that resulted in vertical surface displacement of 1.2 ± 0.2 m. The most recent earthquake is constrained to have occurred after 815 AD, and we have modeled three possible earthquake scenarios constraining the timing of the latest event. Coseismic deformation is characterized by vertical offset of sedimentary contacts distributed over a 10-m-wide central damage zone. Faults were identified where they fracture and offset pebbles in the vertically displaced gravel layers and fracture orientation is consistent with the orientation of the Schafberg fault. This study provides the first constraint on the most recent surface-rupturing earthquake on the Schafberg fault. We cannot rule out that this fault acted as the source of the 1756 Düren earthquake. Our study emphasizes the importance of, and the need for, paleoseismic studies in this and other intracontinental regions, in particular on faults with subtle geomorphic expression that would not typically be recognized as being potentially seismically active. Our study documents textural features in unconsolidated sediment that formed in response to coseismic rupturing of the underlying bedrock fault. We suggest that these features, e.g., abundant oriented transgranular fractures in their context, should be added to the list of criteria used to identify a fault

Una mirada a la situación de la niñez en el Valle del Cauca

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Ana María Osorio

2010-10-01

Full Text Available En este documento identificamos un conjunto de indicadores a nivel departamental y municipal (en la medida en que la información lo permite con perspectiva de niñez, indicadores que facilitan analizar el bienestar y cumplimiento de los derechos de los niños y niñas en distintas áreas: salud, educación, alimentación, vivienda digna, y la exposición a riesgos tempranos como el trabajo y la maternidad. La construcción de indicadores a nivel municipal que reflejan el bienestar y/o el cumplimiento de los derechos, ofrece una oportunidad para obtener una imagen completa de la situación de la niñez en un departamento, y constituye una herramienta sumamente importante en el diseño de la política pública y la focalización del gasto. Los indicadores del Valle del Cauca aquí presentados reflejan inequidades geográficas en la provisión y acceso de servicios sociales básicos; en ellos se evidencian grandes brechas entre municipios frente al promedio departamental y la ciudad de Cali. Los mayores rezagos se concentran en algunos municipios del norte del Valle y el municipio de Buenaventura. Todo esto plantea importantes retos de política pública, e invitan al debate, al análisis y a la visualización de las condiciones de vida de la niñez en el Valle del Cauca.

Una mirada a la situación de la niñez en el Valle del Cauca

Directory of Open Access Journals (Sweden)

Ana María Osorio

2010-01-01

Full Text Available En este documento identificamos un conjunto de indicadores a nivel departamental y municipal (en la medida en que la información lo permite con perspectiva de niñez, indicadores que facilitan analizar el bienestar y cumplimiento de los derechos de los niños y niñas en distintas áreas: salud, educación, alimentación, vivienda digna, y la exposición a riesgos tempranos como el trabajo y la maternidad. La construcción de indicadores a nivel municipal que reflejan el bienestar y/o el cumplimiento de los derechos, ofrece una oportunidad para obtener una imagen completa de la situación de la niñez en un departamento, y constituye una herramienta sumamente importante en el diseño de la política pública y la focalización del gasto. Los indicadores del Valle del Cauca aquí presentados reflejan inequidades geográficas en la provisión y acceso de servicios sociales básicos; en ellos se evidencian grandes brechas entre municipios frente al promedio departamental y la ciudad de Cali. Los mayores rezagos se concentran en algunos municipios del norte del Valle y el municipio de Buenaventura. Todo esto plantea importantes retos de política pública, e invitan al debate, al análisis y a la visualización de las condiciones de vida de la niñez en el Valle del Cauca.

Zeolites of the Valle Central of Costa Rica and its outskirts

International Nuclear Information System (INIS)

Zeledon, Luis Alonso

2004-01-01

19 different species of zeolites have been found in 25 outcrops in the Valle Central of Costa Rica and in the Siquirres region. All the zeolites are secondary minerals and crystallized in little veins and vesicles of the basalts and pyroclastics rocks of the La Cruz and Grifo Alto formations, belonging to the Aguacate Group and the alkaline igneous rocks of Guayacan. The most frequent species of zeolites are stibnite, chabasite, laumontite, mesolite/mordenite, thomsonite, and analcime. Natrolite only was found near to Siquirres. (Author) [es

"Estudio prospectivo de hatos ganaderos, del valle de Ubate, condiciones actuales, limitantes y necesidades de desarrollo para entrar a competir en el mercado internacional"

OpenAIRE

Prieto, Juan Antonio; Uribe Aguado, Manuela; Valdivieso Ruiz, Maria Camila

2011-01-01

El siguiente trabajo titulado “Estudio Prospectivo de hatos ganaderos, del Valle de Ubate, Condiciones Actuales, Limitantes y Necesidades de Desarrollo Para entrar a Competir en el Mercado Internacional” encontrara un ejercicio prospectivo orientado a establecer posibles escenarios futuros para los ganaderos, productores de leche del Valle de Ubate, a entrar nuevos mercados como el europeo y americano al mercado Colombiano, así mismo propone un análisis de las variables relevantes de las co...

ZONAS FRÍAS EN EL VALLE DEL RÍO NEUQUÉN: SU DETECCIÓN MEDIANTE IMÁGENES NOAA-AVHRR

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Marisa Cogliati

2003-12-01

Full Text Available El valle inferior del río Neuquén se encuentra incluido en la zona agrícola conocida como Alto Valle del río Negro (AVRN que a pesar de su denominación, incluye además los valles inferiores de los ríos Limay y Neuquén. En esta región se destaca una intensa actividad frutihortícola. Las heladas tardías (que ocurren en los meses de setiembre y octubre constituyen riesgos importantes para dicha actividad llegando incluso a ocasionar grandes pérdidas económicas. Debido a ello, en los valles, se invierten grandes sumas de dinero en la lucha contra las heladas. El Alto Valle del Río Negro es una región con características propias, por los recursos del suelo y subsuelo, por el avance de las ciudades, el numero de habitantes y la tecnificación. La zona cultivada ocupa terrazas fluviales y el abastecimiento de agua se realiza por medio del riego artificial. La superficie regada es de 100000 has. El estudio de las características del clima de la región así como de cada una de las variables climáticas tiene implicancias que poco a poco han sido consideradas por los diferentes agentes del sector productivo. Esto se ve reflejado en la cantidad de estaciones meteorológicas automáticas que han sido adquiridas en la región, tanto por el sector privado como por los organismos públicos relacionados al sector productivo fruti-hortícola (INTA, FUNBAPA; UNC, etc.. Desde hace unos años, se han efectuado distintos esfuerzos aislados desde todas esas instituciones para reunir información y analizar las características propias de la región, sin que se hayan coordinado esfuerzos. Los estudios realizados presentan en su mayoría el estudio de datos de las estaciones meteorológicas convencionales pertenecientes al Servicio Meteorológico Nacional y a la Facultad de Ciencias Agrarias de la Universidad Nacional del Comahue con registros de aproximadamente 30 años, pero no presentan un estudio espacial del tema, sino que definen ciertas

Minerale geme asociate genetic ofiolitelor mezozoice si gheizeritelor neogene, din Muntii Apuseni de Sud

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Ioan Mârza

2000-04-01

Full Text Available The paper studies the geological formations of the Geoagiu- Hărţăgani- Vălişoara- Brad region (Southern Apuseni Mountains focusing on the content in gems minerals. Based on the field and laboratory reasearch, several perimeters of geological interest have been identified: Luncoiu Valley- Lunga Valley, Vălişoara Valley- Orăzii Valley, Baiţa-Crăciuneşti, Hărţăgani and Sanatoriu (Brad. Geologically, the minerals of gem quality (quartz, chalcedony, jasper and they associate genetically and spatially with ophiolites, with the exception of the Brad silicolite- gems which represent geyserites generated by the neogene volcanism.

10Be in rhodochrosite nodules from Neogene sediments along the Galapagos Ridge, equatorial Pacific

International Nuclear Information System (INIS)

Aldahan, A.; Morad, S.; Possnert, G.; Sturesson, U.; ElSaiy, A.

2010-01-01

Microcrystalline, calcian rhodochrosite occurs as nodules around burrows in late Neogene pelagic sediments from the Galapagos Ridge in the Guatemala Basin, eastern equatorial Pacific (DSDP Leg 68; Site 503). 10 Be isotope revealed that the rhodochrosite nodules have formed under growth conditions much faster than those reported for Fe-Mn nodules. The overall REE patterns of the nodules and host pelagic sediments indicate element derivation mainly from marine pore water. However, variations in the shale normalised Eu values suggest influx of hydrothermal fluids into mounds area at Galapagos, which is also evidenced by the similar minor and major element contents in the nodules and host sediments.

RASGOS GEOGRÁFICOS DEL VALLE DEL RIO AGRIO INFERIOR.

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Celia Torren

1993-12-01

Full Text Available El presente artículo es una síntesis del trabajo "Rasgos Geográficos del Valle del Río Agrio Inferior, el cual es un estudio de base para el conocimiento de la geografía de la región: - apoyando el esfuerzo que está realizando la población del área para lograr una identidad propia y una definitiva integración al contexto provincial; - aportando al proyecto "Rescate Arqueológico en Quili Malal, Neuquén" (subsidiado por CONICET y UNESCO, cuya dirección está a cargo de la profesora Susana Rodríguez de la U.N.C., a través de la confección del mapa geomorfológico del área; y - contribuyendo a los estudios que resultan necesarios ante la construcción de una obra hidroeléctrica de la magnitud de "El Chihuido I", emprendimiento que será llevado a cabo por Agua y Energía eléctrica de la Nación. Los límites del área estudiada fueron establecidos teniendo en cuenta el área del valle inferior del Río Agrio que será completamente inundada por el futuro embalse de la represa "El Chihuido I", a emplazarse 5,5 Km aguas abajo de la confluencia de los ríos Agrio y Neuquén. Además de esta área de afectación directa se tomó también una zona de perilago estrechamente vinculada a la anterior. De esta manera los límites este y oeste quedaron establecidos por la confluencia de los ríos antes mencionados y la localidad de Bajada del Agrio, respectivamente.

Le Paléolithique de la Vallée de l'Arros.

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Jean Barrage

1993-01-01

Full Text Available Entre los ríos Adour y Neste, en los Pirineos centrales, el valle medio y superior del río Arros fue ocupado episódicamente por los hombres prehistóricos : En el Paleolítico Inferior con un Achelense sobre cuarcita, en el Paleolítico Medio con estaciones Mustenienses en los altos de las colinas y Magdaleniense clásico en las cuevas de Lomné y Espêche.

Balance hidrológico en los valles de Tambo, Moquegua e Ilo

OpenAIRE

Instituto Nacional de Desarrollo

2001-01-01

Realiza el Balance hidrológico en los valles de Tambo, Moquegua e Ilo a fin de conocer la problemática del recurso hídrico en la dicha zona ante la posibilidad de otorgar derechos de uso de agua para el desarrollo de un proyecto minero y contar con un documento técnico que permita analizar, evaluar y proponer alternativas de solución a posibles conflictos en torno al aprovechamiento del agua.

Ground Motion Relations for the Upper Rhine Graben

Science.gov (United States)

Calbini, V.; Granet, M.; Camelbeeck, T.

2006-12-01

Earthquake in Europe are primarily located within the Euro-Mediterranean domain. However, the Upper Rhine Graben (URG) region regularly suffers earthquakes which are felt physically by inhabitants and cause damage to private property and the industrial infrastructure. In 1356, a major earthquake (I0 = X) destroyed part of the city of Basel. Recently, several events having M > 5 have shaken this area. In the framework of an INTERREG III project funded by the European community, a microzonation study has been achieved across the "three borders" area including the cities of Basel and Mulhouse. In particular, the ground motion was studied. The URG, which belongs to the ECRIS (European Cenozoic Rift System), is characterized by rift-related sedimentary basins with several hundreds meters of tertiary sediments overlaying the basement. Such a subsurface geology leads to strong site effects. Predictive attenuation laws and their related uncertainties are evaluated considering strong motions records and velocimetric records from small to moderate local events (Magnitude ranging 3

Mito, historia e identidad en Cachi (Valles Calchaquíes, Salta

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Paula Lanusse

2010-07-01

Full Text Available El artículo trata acerca de la memoria de los antiguos en una localidad del sudoeste de la provincia de Salta (Cachi, región de los Valles Calchaquíes. En esta área la población aborigen fue sometida en el siglo diecisiete, iniciándose luego un proceso ambivalente de invisibilización étnica y persistencia de marcaciones indígenas en la definición de la singularidad de sujetos subalternos. A partir del análisis de relatos orales y de prácticas espaciales de estos sujetos cacheños, se busca interpretar el modo y el significado en que construyen una memoria de los antiguos, enfatizando las ideas de tiempo y espacio implicadas en esas historias y reflexionando acerca del correlato identitario que presuponen.This article is about memory of los antiguos (the ancients ones in a southwestern locale of Salta (Valles Calchaquíes, Salta, Argentina. In this area the aboriginal people was subdued during the 17th century following an ambivalent process of ethnic invisibilization and persistent use of ethnic markers to define the subaltern population up to the present. By analyzing Cachi subalterns' oral narratives and spatial practices I attempt to interpret the modes in which they construe a memory of los antiguos, paying attention to the notions of space and time contained therein and the identity correlate they presuppose.

Developments of ozone generation using dielectric barrier discharge at the Universidad del Valle

OpenAIRE

Echeverry-Ibarra, Diego F.

2013-01-01

This paper presents the research results related to ozone technology using dielectric barrier discharge DBD, obtained at the Universidad del Valle. Particular emphasis is placed on increasing efficiency, the modeling of the surface dielectric barrier discharge generator and the control technique which modifies the relation production vs. efficiency of the generators. Finally, the ozone applications worked at the university are presented. The current state of these developments is promising fo...

Posoqoypata, un cementerio Wari en el valle de Ayacucho, Perú

OpenAIRE

Valdez, Lidio M.; Valdez, J. Ernesto; Bettcher, Katrina J.

2015-01-01

Recientemente efectuamos un trabajo de rescate arqueológico en un cementerio Wari en el valle de Ayacucho. Dicho trabajo permitió el descubrimiento de formas mortuarias totalmente novedosas para la región y para la cultura Wari en particular. La primera consiste en una cámara funeraria de forma rectangular, con un acceso orientado hacia el lado este, y que contenía los restos de varios individuos. La segunda tiene la forma de una pequeña cista de forma cilíndrica que contenía los restos de un...

Política pública de la migración en el Departamento del Valle del Cauca. ¿Cómo se está tratando el tema de la migración internacional, en el Departamento del Valle del Cauca hasta el 2009?

Directory of Open Access Journals (Sweden)

Lorena López López

2011-08-01

Full Text Available El presente documento de trabajo se basa en la tesis de grado, presentada en la Universidad Icesi de Cali, bajo el mismo título del presente artículo. El texto aborda la Política Integral Migratoria (PIM de Colombia y sus implicaciones en el departamento del Valle del Cauca. El documento está dividido en cuatro temas principales. Primero, se presenta el marco teórico, enfocado, particularmente, en el concepto de migración internacional, el cual se analiza desde distintos puntos de vista y autores. Segundo, se retoman los últimos 30 años de proceso histórico migratorio desde el departamento del Valle del Cauca al exterior. Tercero, se analiza el documento Conpes 3603, emitido por el Gobierno Nacional, en cabeza del Ministerio de Relaciones Exteriores, y se escruta sobre la influencia de este en las políticas formuladas e implementadas en el departamento. Cuarto, se enumeran algunas de las organizaciones gubernamentales, y no gubernamentales, más relevantes con las cuales trabaja el gobierno del Valle del Cauca para lograr el desarrollo de la Política Integral Migratoria (PIM en el departamento. Finalmente, el presente artículo pretende brindar algunas conclusiones, a modo de reflexión, sobre los retos que enfrenta la Política Integral Migratoria (PIM en el departamento.

Structure of the Hat Creek graben region: Implications for the structure of the Hat Creek graben and transfer of right-lateral shear from the Walker Lane north of Lassen Peak, northern California, from gravity and magnetic anomalies

Science.gov (United States)

Langenheim, Victoria; Jachens, Robert C.; Clynne, Michael A.; Muffler, L. J. Patrick

2016-01-01

Interpretation of magnetic and new gravity data provides constraints on the geometry of the Hat Creek Fault, the amount of right-lateral offset in the area between Mt. Shasta and Lassen Peak, and confirmation of the influence of pre-existing structure on Quaternary faulting. Neogene volcanic rocks coincide with short-wavelength magnetic anomalies of both normal and reversed polarity, whereas a markedly smoother magnetic field occurs over the Klamath Mountains and its Paleogene cover. Although the magnetic field over the Neogene volcanic rocks is complex, the Hat Creek Fault, which is one of the most prominent normal faults in the region and forms the eastern margin of the Hat Creek Valley, is marked by the eastern edge of a north-trending magnetic and gravity high 20-30 km long. Modeling of these anomalies indicates that the fault is a steeply dipping (~75-85°) structure. The spatial relationship of the fault as modeled by the potential-field data, the youngest strand of the fault, and relocated seismicity suggests that deformation continues to step westward across the valley, consistent with a component of right-lateral slip in an extensional environment. Filtered aeromagnetic data highlight a concealed magnetic body of Mesozoic or older age north of Hat Creek Valley. The body’s northwest margin strikes northeast and is linear over a distance of ~40 km. Within the resolution of the aeromagnetic data (1-2 km), we discern no right-lateral offset of this body. Furthermore, Quaternary faults change strike or appear to end, as if to avoid this concealed magnetic body and to pass along its southeast edge, suggesting that pre-existing crustal structure influenced younger faulting, as previously proposed based on gravity data.

A Paleogeographic and Depositional Model for the Neogene Fluvial Succession, Pishin Belt, Northwest Pakistan: Effect of Post Collisional Tectonics on Sedimentation in a Peripheral Foreland Setting

DEFF Research Database (Denmark)

Kasi, Aimal Khan; Kassi, Akhtar Muhammad; Umar, Muhammad

2018-01-01

. During the Early Miocene, subaerial sedimentation started after the final closure of the Katawaz Remnant Ocean. Based on detailed field data, twelve facies were recognized in Neogene successions exposed in the Pishin Belt. These facies were further organized into four facies associations i.e. channels......‐story sandstone and/or conglomerate channels, lateral accretion surfaces (point bars) and alluvial fans. Neogene sedimentation in the Pishin Belt was mainly controlled by active tectonism and thrusting in response to the oblique collision of the Indian Plate with the Afghan Block of the Eurasian Plate along......, crevasse splay, natural levee and floodplain facies associations. Facies associations and variations provided ample evidence to recognize a number of fluvial architectural components in the succession e.g., low‐sinuosity sandy braided river, mixed‐load meandering, high‐sinuosity meandering channels, single...

Posoqoypata, un cementerio wari en el valle de Ayacucho, Perú

Directory of Open Access Journals (Sweden)

2001-01-01

Full Text Available POSOQOYPATA, UN CIMETIÈRE WARI DE LA VALLEE D’AYACUCHO, PEROU. Nous avons récemment effectué un travail de sauvetage arquéologique dans un cimetière Wari de la vallée d’Ayacucho, ce qui a permis la mise à jour de deux formes mortuaires totalement nouvelles pour la région, et pour la culture Wari plus précisemment. La première consiste en une chambre funéraire de forme rectangulaire, avec un accès orienté à l’Est, et qui contenait les restes de plusieurs individus. La seconde est une petite sépulture en pierres de forme cylindrique qui contenait les restes d’un individu. Ce texte décrit les deux formes mortuaires et les compare avec les structures mortuaires Wari fouillées jusqu’à aujourd’hui dans la vallée d’Ayacucho. Étant donné qu’il est évident que la première forme mortuaire a été accessible, nous discutons ici les conséquences possibles pour l’adoration du corps des ancêtres, qui étaient conservés dans des structures mortuaires accessibles, cet élément étant considéré comme un aspect important de l’ayllu de l’époque Inka. Recientemente efectuamos un trabajo de rescate arqueológico en un cementerio Wari en el valle de Ayacucho. Dicho trabajo permitió el descubrimiento de formas mortuarias totalmente novedosas para la región y para la cultura Wari en particular. La primera consiste en una cámara funeraria de forma rectangular, con un acceso orientado hacia el lado este, y que contenía los restos de varios individuos. La segunda tiene la forma de una pequeña cista de forma cilíndrica que contenía los restos de un individuo. En este ensayo describimos ambas formas mortuarias y comparamos con las estructuras mortuarias Wari excavadas a la fecha en el valle de Ayacucho. Por cuanto la primera forma mortuaria fue evidentemente accesible, también discutimos sus posibles implicancias en torno a la adoración del cuerpo de los ancestros. Esto considerando que un aspecto importante del ayllu de la

Incidencia del deterioro progresivo del arbolado urbano en el Valle de Aburrá, Colombia

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Hector Ivan Restrepo Orozco

2015-07-01

Full Text Available El arbolado urbano de los municipios del Valle de Aburrá, Colombia, está evidenciando deterioro y muerte por estrés hídrico y térmico, contaminación atmosférica, urbanización y ataques de plagas y enfermedades. Se realizó un muestreo de 11 710 individuos de 25 especies de árboles y palmas en el área metropolitana del Valle de Aburrá, con el propósito de registrar síntomas de deterioro progresivo (DP como marchitez de ramas y secamiento descendente. Se estimó un modelo logit multifactorial que relaciona la incidencia del DP con características dasométricas de los individuos, el sitio de siembra y el número de afectaciones. Se encontraron 720 individuos con DP (incidencia de 6.1%. Los modelos logit tuvieron un ajuste satisfactorio a los datos y evidenciaron que existe una relación estadísticamente significativa entre la incidencia del deterioro de árboles y el diámetro del árbol, su ubicación (municipio, especie, sitio de siembra (zona verde, piso duro, alcorque y presencia de otras afectaciones.

El saber de la partera tradicional del valle del río Cimitarra: cuidando la vida

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CELMIRA LAZA VÁSQUEZ

2009-12-01

Full Text Available Para la recolección y análisis de la información se utilizaron la Etnografía focalizada y la técnica de Spradley y la teoría de la diversidad y la universalidad de los cuidados culturales de Leininger se tomó como referente teórico. Su objetivo fue describir los cuidados que brindaban las parteras tradicionales a partir de creencias y prácticas en las mujeres durante el parto en la zona rural de la región del valle del río Cimitarra, Magdalena Medio. El estudio se desarrolló en el valle del río Cimitarra y la ciudad de Barrancabermeja. Participaron siete parteras tradicionales y se recolectaron los datos mediante entrevista etnográfica y observación participante entre los años 2007 y 2008. El tema central es " El saber de la partera tradicional del valle del río Cimitarra: cuidando la vida" y cinco dominios culturales: alistarse para la atención del mismo, identificar el momento del parto, ayudar a la mujer a parir, proteger al bebé después del nacimiento y proteger a la mujer después del nacimiento. Cuidar la vida se relaciona con la necesidad de " sobrevivir" a pesar de la guerra, la violencia y el abandono estatal. Las acciones de cuidado se fundan en creencias culturales, la cotidianidad del trabajo del campo, la tradición oral y la invocación divina en medio del complejo contexto ambiental, la incertidumbre del conocmiento y el miedo a problemas legales.

Analysis of soft-sediment deformation structures in Neogene fluvio-lacustrine deposits of Çaybağı Formation, Eastern Turkey

Science.gov (United States)

Koç Taşgin, Calibe; Türkmen, İbrahim

2009-06-01

During the Neogene, both strike-slip and extensional regimes coexisted in eastern Turkey and, a number of fault-bounded basins associated with the East Anatolian Fault System developed. The Çaybağı Formation (Late Miocene-Early Pliocene) deposited in one of these basins consists of fluvio-lacustrine deposits. Numerous soft-sediment deformation structures are encountered in this formation, particularly in conglomerates, medium- to coarse-grained tuffaceous sandstones and claystones: folded structures (slumps, convolute laminations, and simple recumbent folds), water-escape structures (intruded sands, internal cusps, interpenetrative cusps and sand volcanoes), and load structures (load casts, pseudonodules, flame structures, and pillow structures). These structures are produced by liquefaction and/or fluidization of the unconsolidated sediments during a seismic shock. Consequently, the existence of seismically-induced deformation structures in the Çaybağı Formation and the association with a Neogene intraformational unconformity, growth faults, and reverse faults in the Çaybağı basin attest to the tectonic activity in this area during the Late Miocene and Early Pliocene. The East Anatolian Fault System, in particular the Uluova fault zone, is the most probable seismogenic source. Earthquakes with a magnitude of over 5 in the Richter scale can be postulated.

Studies on the Neogene Tertiary strata distributed in the central part of Tottori prefecture

International Nuclear Information System (INIS)

Yoshitani, Akihiko; Yoshizawa, Junko.

1978-01-01

The Neogene Tertiary strata, distributed in the central part of Tottori Prefecture, are volcano-stratigraphically classified, as shown in Figure 3. The Miocene strata are divided into Ojika formation and Mitoku formation in ascending order. Ojika formation, composed of plagio-rhyolitic pyroclastics and lavas, abuts against the basement rocks. Furthermore, some breaccias derived from the talus basal conglomerate beds are found in Ojika formation. Mitoku formation abuts both against the basement rocks and Ojika formation, and sometimes overlaps on the basement rocks. From the investigation into the Miocene strata, it is clarified that the depression took place prior to the volcanic activities at the earliest stage of the present Miocene sedimentary basin. (author)

Estudios sobre la enfermedad de Carrión en el valle interandino del Mantaro: I. Observaciones entomológicas

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Aristides Herrer

1960-01-01

Full Text Available Durante los primeros meses de 1959 se presentó una epidemia de la enfermedad de Carrión o verruga peruana en el valle interandino del Mantaro, de preferencia en localidades próximas a la de Anco. Las investigaciones entomológicas realizadas al respecto han permitido conocer la existencia en dicha zona de dos especies de titiras, el Phlebotomus pescei y el P. bicornutus n. sp.; en cambio no se ha encontrado al P. verrucarum, conocido vector de la enfermedad de Carrión en el Perú. Las dos especies de titiras obtenidas en el Mantaro ingresan con frecuencia a las habitaciones humanas y se alimentan sobre el hombre y varias especies de animales, tanto domésticas como salvajes. Hay una marcada diferencia en cuanto a la distribución altitudinal de las dos especies de titiras del Mantaro. El P. bicornutus es abundante en las localidades de menor altitud sobre el nivel del mar y parece que el límite superior de su distribución se encuentra alrededor de los 2,600 metros. El P. pescei, en cambio, es una titira de mayor altura. Por debajo de los 2,400 metros es sumamente rara, entretanto que se le encuentra con mayor frecuencia entre los 2,600 y los 3,000 metros; a partir de esta altitud nuevamente se torna escasa hasta los 3,300 metros, altura máxima donde se le ha encontrado. Los lugares donde se ha verificado la mayoría de los casos de verruga, en el valle del Mantaro, por la altitud corresponden al de la distribución del P. pescei, por lo que es de suponer dicha titira actúe de trasmisora de la enfermedad de Carrión en el referido valle del Mantaro. En el valle del Mantaro, a niveles superiores al de la respectiva zona verrucógena existe una considerable población autóctona, parte de la cual anualmente desciende por espacio de algunas semanas a lugares donde la enfermedad de Carrión es endémica, lo que da lugar a numerosos casos de verruga. En noviembre de 1958 el Servicio Nacional de Erradicación de la Malaria aplicó el

Distribución e identificación de especies hospedantes de Heterodera glycines Ichinohe raza 3 en el Valle del Cauca

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Varón de Agudelo Francia

1988-06-01

Full Text Available Se dividió la parte plana del Valle del Cauca en tres zonas (norte, centro y sur, habiéndose visitado 33 fincas. En la zona norte las malezas con mayor porcentaje de frecuencia y distribución en los cultivos de soya fueron Digitaria horizontalis, Echinochloa colonum y Leptochloa filiformis; en la zona centro Ipomoea hirta, Amaranthus dubius y Echinochloa colonum y en la zona sur predominaron Ipomoea hirta, Portulaca oleracea Cyperus rotundus. Los análisis de muestras de suelo y raíces indicaron que H. glycines se encuentra distribuido en todo el Valle del Cauca, presentando la zona sur (Candelaria, Palmira y Puerto Tejada las mayores poblaciones. Entre las especies evaluadas (malezas, cultivos, leguminosas forrajeras y silvestres, solamente Glycine max y Phaseolus vulgaris se consideraron como susceptibles a H. glycines raza 3. y P. angularis y P. multiflora permitieron muy poca infección y multiplicación del nemátodo.A nematode recognition of Heterodera glycines was focused on crops of soybean. Valle del Cauca was divided in three zones (northen, central and southern and 33 farms were visited. The results of the analysis on samples of soils and roots showe that Heterodera glycines is scattered throughout Valle del Cauca, being the southern zone (Palmira, Candelaria and Puerto Tejada the one having the highest standards in nematode population. Weeds showing a greater frequency percentage were : Digitaria horizontalis, Echinochloa colonum and Leptochloa filiformis, in the northen zone; Ipomoea hirta, Amaranthus dubius and Echinochloa colonum, in the central zone, and Ipomoea hirta, Portulaca oleracea and Cyperus rotundus, in the southern zone , From among the whole species evaluated (weeds, crops, leguminous a n d fodder plants, Glycine max and Phaseolus vulgaris were considered to be susceptible to H. Glycines race 3. Phaseolus angularis y P. multiflora let low population levels.

Outcrop analogue study of Permocarboniferous geothermal sandstone reservoir formations (northern Upper Rhine Graben, Germany): impact of mineral content, depositional environment and diagenesis on petrophysical properties

Science.gov (United States)

Aretz, Achim; Bär, Kristian; Götz, Annette E.; Sass, Ingo

2016-07-01

The Permocarboniferous siliciclastic formations represent the largest hydrothermal reservoir in the northern Upper Rhine Graben in SW Germany and have so far been investigated in large-scale studies only. The Cenozoic Upper Rhine Graben crosses the Permocarboniferous Saar-Nahe Basin, a Variscan intramontane molasse basin. Due to the subsidence in this graben structure, the top of the up to 2-km-thick Permocarboniferous is located at a depth of 600-2900 m and is overlain by Tertiary and Quaternary sediments. At this depth, the reservoir temperatures exceed 150 °C, which are sufficient for geothermal electricity generation with binary power plants. To further assess the potential of this geothermal reservoir, detailed information on thermophysical and hydraulic properties of the different lithostratigraphical units and their depositional environment is essential. Here, we present an integrated study of outcrop analogues and drill core material. In total, 850 outcrop samples were analyzed, measuring porosity, permeability, thermal conductivity and thermal diffusivity. Furthermore, 62 plugs were taken from drillings that encountered or intersected the Permocarboniferous at depths between 1800 and 2900 m. Petrographic analysis of 155 thin sections of outcrop samples and samples taken from reservoir depth was conducted to quantify the mineral composition, sorting and rounding of grains and the kind of cementation. Its influence on porosity, permeability, the degree of compaction and illitization was quantified. Three parameters influencing the reservoir properties of the Permocarboniferous were detected. The strongest and most destructive influence on reservoir quality is related to late diagenetic processes. An illitic and kaolinitic cementation and impregnation of bitumina document CO2- and CH4-rich acidic pore water conditions, which are interpreted as fluids that migrated along a hydraulic contact from an underlying Carboniferous hydrocarbon source rock. Migrating

The Jurassic of Denmark and Greenland: Sedimentology and sequence stratigraphy of the Bryne and Lulu Formations, Middle Jurassic, northern Danish Central Graben

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Andsbjerg, Jan

2003-10-01

or lacustrine mudstones. The unconformity that separates the alluvial plain deposits of the lower Bryne Formation from the estuary deposits of the upper Bryne Formation is interpreted as a sequence boundary that bounds a system of incised valleys in the western and southern parts of the basin. Sequence boundaries in the Lulu Formation are situated at the top of progradational shoreface units or at the base of estuarine channels. Maximum flooding surfaces are located within marine or lagoonal mudstone units. Marine highstand deposits are partitioned seawards, in the eastern part of the basin, whereas paralic transgressive deposits are partitioned landwards, in the west. This marked sediment artitioning in the uppermost part of the succession resulted from the alternation of episodes of fault-induced half-graben subsidence with periods of slow uniform subsidence.

Primer registro de Phyllodactylus sentosus (Squamata: Phyllodactylidae para el valle del río Chillón, Lima, Perú

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Diego Olivera

2016-12-01

Full Text Available El gecko de Lima Phyllodactylus sentosus (Dixon & Huey, 1970 identificado como en peligro crítico de extinción ha sido registrado sólo en algunas localidades entre los valles de los ríos Rímac y Lurín, en el centro y sur de la ciudad de Lima, Región Lima, sin embargo, su distribución hacia el norte no está documentada. En el presente trabajo se reporta por primera vez la presencia de P. sentosus en la Huaca Tambo Inga, ubicada en el margen derecho del valle del río Chillón en el distrito de Puente Piedra, extendiendo su distribución 19 km al noreste.

{sup 10}Be in rhodochrosite nodules from Neogene sediments along the Galapagos Ridge, equatorial Pacific

Energy Technology Data Exchange (ETDEWEB)

Aldahan, A., E-mail: ala.aldahan@geo.uu.s [Department of Earth Sciences, Uppsala University, Uppsala (Sweden); Department of Geology, United Arab Emirates University, Al Ain (United Arab Emirates); Morad, S. [Department of Earth Sciences, Uppsala University, Uppsala (Sweden); Department of Petroleum Geosciences, Petroleum Institute, Abu Dhabi (United Arab Emirates); Possnert, G. [Tandem Laboratory, Uppsala University, Uppsala (Sweden); Sturesson, U. [Department of Earth Sciences, Uppsala University, Uppsala (Sweden); ElSaiy, A. [Department of Geology, United Arab Emirates University, Al Ain (United Arab Emirates)

2010-04-15

Microcrystalline, calcian rhodochrosite occurs as nodules around burrows in late Neogene pelagic sediments from the Galapagos Ridge in the Guatemala Basin, eastern equatorial Pacific (DSDP Leg 68; Site 503). {sup 10}Be isotope revealed that the rhodochrosite nodules have formed under growth conditions much faster than those reported for Fe-Mn nodules. The overall REE patterns of the nodules and host pelagic sediments indicate element derivation mainly from marine pore water. However, variations in the shale normalised Eu values suggest influx of hydrothermal fluids into mounds area at Galapagos, which is also evidenced by the similar minor and major element contents in the nodules and host sediments.

Stable isotopic mass balance in sandstone-shale couplets. An example from the Neogene Pannonian Basin

International Nuclear Information System (INIS)

Matyas, J.; Geologisches Institut.

1996-01-01

Oxygen isotopic ratios of carbonate cements in the Neogene sandstones of the Pannonian Basin show distinct variations: early calcites 3-6 per mille lighter than the late calcites from the same location and depth. This shift is thought to be related to the isotopically heavy oxygen released from the mixed-layer illite/smectite during illitisation. For sandstones dominated by compactional flow, closed system mass balance calculations predict an isotopic shift comparable to that deducted from petrographic and geochemical observations. The model suggests that variations of geothermal gradient has little effect on isotopic evolution; much more significant is the sandstone: shale ratio in the couplets. (author)

Contribution to the Investigation of Structure and Origin of the East African Graben by Gravimetry

Institute of Scientific and Technical Information of China (English)

Tondozi Keto; LIU Tianyou

2005-01-01

For our investigation we have 235 measurements done in the east part of Democratic Republic of Congo by P. Herrinck during a magnetic survey including the graben region from the parallel joining Goma city and Mahagi city, the region between Albert and Aka lakes, and the route from Aba to Kinsagani. During the surveys the density of recording points has been selected according to the importance of anomalies. In this way, the offset was 1 km where the disturbance was high in Goma city and 20 km have been sufficient along the route from Aba to Kinsagani. For the topographic and isostatic reductions only one cartographic document has been chosen that was the international map of the scale 1/1 000 000 which presents a certain characteristic of homogeneity.

Yacimientos de Celestina en la Plataforma Valles-San Luis Potosí

OpenAIRE

Rocha Rocha, Macario

2008-01-01

En la zona de estudio, la Plataforma Valles-San Luis Potosí (PVSLP), existen depósitos de celestina; las características geotectónicas de la zona, hacen pensar que estos depósitos se asocian con evaporitas del Jurásico Superior-Cretácico Inferior. La mineralización de celestina arma en la Formación El Abra y en menor grado la Formación Indidura, en forma de vetas, mantos, zonas de brecha y cuerpos irregulares. La mineralogía consiste básicamente de celestina y algunos minerales...

Relaciones productivas y configuración de la política sectorial en el Valle de Aburrá

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Marleny Cardona Acevedo

2001-01-01

el artículo muestra la influencia de los procesos productivos y las condiciones tecnológicas de las empresas en la capacidad directiva y en la organización del trabajo en empresas industriales asentadas en el Valle de Aburrá, Colombia.

Producción y desarrollo de nueve variedades de naranja Citrus sinensis (L. Osbeck en la zona plana del Valle del Cauca

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Salazar C. Raúl

1990-12-01

Full Text Available En árboles de naranja de cinco años injertados sobre mandarina Cleopatra, se evaluaron nueve variedades sembradas en un diseño experimental de bloques completos al azar. El crecimiento de los frutos presentó las tres fases típicas, con duración variable dependiendo de la variedad: lento, crecimiento acelerado y estabilización. Los máximos crecimientos se obtuvieron en las variedades Old Vini, Valencia y Valle Washington. En todas las variedades los sólidos solubles disminuyeron y el porcentaje de acidez aumentó hasta ciertos límites con la edad del fruto. Considerando como momento óptimo para iniciar la cosecha una relación de sólidos solubles: acidez de 9.5:1, la más temprana fue la Valle Washington (7.5 meses, intermedias Old Vini y Australia Navel y la más tardía García Valencia. Todas las variedades presentaron contenidos de jugo mayores del 50 % Y color atractivo de la pulpa. El color más atractivo de la corteza se obtuvo en Parson Brown (97.5 % amarillo, las otras variedades fluctuaron entre 48 y 79%. Todas las variedades tuvieron menos de seis semillas por fruto. Se presentaron dos épocas de cosecha y las variedades con mayor producción: Hamlin, García Valencia y Pineapple tuvieron la mayor variación mensual. La mejor alternativa sembrando 90% de variedades para industria y 10 % para mesa se obtuvo con las variedades Pineapple, Hamlin, Parson Brown, Valle Washington y Old Vini.Five years old orange trees, were grafted on Cleopatra scions of nine cultivars planted in a completely randomized block design were evaluated. Fruit growths presented three typical phases of variable lenght, depending on the cultivar: slow , rapid and stable growth rates. Largest growth were observed in the old Vini, Valencia and Valle Washington cultivars. In all cases total soluble solid contents and acidity increased, up to certain point, with fruit age. Considering that the optimum time to iniciate cropping is when the relationship

Paisajes del Valle medio del Guadalquivir cordobés: Funcionalidad y cambios

OpenAIRE

Martín Torres Márquez

2013-01-01

RESUMEN: Los tradicionales paisajes agrarios del Valle cordobés, ligados a la presencia del Guadalquivir, han sido importantes y tempranas áreas de modernización económica, gracias al desarrollo de la agricultura, el regadío y la industrialización. Sin embargo, esas funciones agrarias, antaño inseparables de la identidad paisajística de los ruedos y el extrarradio de Córdoba, se hallan en retroceso desde el último tercio del siglo XX, un retroceso provocado por la expansión de la ciudad difu...

Paisajes del Valle medio del Guadalquivir cordobés: Funcionalidad y cambios

OpenAIRE

Torres-Márquez, Martín

2013-01-01

Los tradicionales paisajes agrarios del Valle cordobés, ligados a la presencia del Guadalquivir, han sido importantes y tempranas áreas de modernización económica, gracias al desarrollo de la agricultura, el regadío y la industrialización. Sin embargo, esas funciones agrarias, antaño insepa- rables de la identidad paisajística de los ruedos y el extrarradio de Córdoba, se hallan en retroceso desde el último tercio del siglo XX, un retroceso provocado por la expansión de la ciud...

Thermal environment characterization for the bovine cattle ranching in the Valle del Cauca, Colombia

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Raúl Andres Molina Benavides

2016-10-01

Full Text Available The influence of climate on animal behavior has been demonstrated for many years. Climatic variables such as temperature (T, ° C, relative humidity (RH, %, solar radiation (SR, W / m2 and wind speed (WS, m / s, outside their normal range, can displace ruminants of their comfort zone, which can results in negative impact on their productivity and reproduction behavior. In order to characterize the thermal environment of bovine cattle ranching in the Valle del Cauca department, two biometeorological indexes (heat load index for dairy cows and meat cattle were performed to develop an animal - environment relationship. The indexes were applied to the most representative Valle del Cauca department climatic ranges (T = 20-35; RH = 60-100; WS = 0-10, finding that for dairy cows under the mentioned conditions of T> 23, RH> 80 and 0 WS, starting to show signals of heat stress, while for beef cattle starts with T> 25, RH> 60 and WS <1.5. In conclusion, these indexes are useful tools to determine the degree of heat stress that may occur on farms during certain times of day for certain months of the year, helping to plan actions to control its effect in cattle and subsequently, mitigate the impacts on their productive and reproductive performance.

Volcanic Structures Within Niger and Dao Valles, Mars, and Implications for Outflow Channel Evolution and Hellas Basin Rim Development

Science.gov (United States)

Korteniemi, J.; Kukkonen, S.

2018-04-01

Outflow channel formation on the eastern Hellas rim region is traditionally thought to have been triggered by activity phases of the nearby volcanoes Hadriacus and Tyrrhenus Montes: As a result of volcanic heating subsurface volatiles were mobilized. It is, however, under debate, whether eastern Hellas volcanism was in fact more extensive, and if there were volcanic centers separate from the identified central volcanoes. This work describes previously unrecognized structures in the Niger-Dao Valles outflow channel complex. We interpret them as volcanic edifices: cones, a shield, and a caldera. The structures provide evidence of an additional volcanic center within the valles and indicate volcanic activity both prior to and following the formation of the outflow events. They expand the extent, type, and duration of volcanic activity in the Circum-Hellas Volcanic Province and provide new information on interaction between volcanism and fluvial activity.

Impacto de la calidad total como teoría de la gestión en las sociedades anónimas del Valle de Aburrá

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Omar de Jesús González

1996-02-01

Full Text Available RESUMEN El objetivo general de este trabajo es Determinar el Impacto de la calidad total como teoría de la gestión en las sociedades anónimas  del Valle de Aburrá. Específicamente el trabajo busca determinar cuántas S.A. del Valle de Aburrá, afiliadas a la corporación  Calidad y/o al Grupo Antioquia  para el Mejoramiento Continuo, han estructurado o están estrucutrando un plan estretégico de Calidad Total.

Sedimentology of the Upper Maastrichtian chalk, Danish Central Graben. M-10X (Dan Field), E-5X (Tyra SE Field) facies and core logs

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Ineson, J.R.

2004-07-01

Based on detailed logs presented here at 1:10, the cored Upper Maastrichtian succession of the M-10X (Dan Field) and E-5X (Tyra SE Field) wells in the southern Danish Central Graben is subdivided into eight lithofacies and five ichnofabrics. The dominant bioturbated or laminated chalk mudstones and subordinate sparse skeletal wackestones are largely the result of pelagic carbonate production, sedimented by suspension settling and small volume, low density turbidity currents. Evidence of winnowing/reduced sedimentation rates is yielded by rare incipient hardgrounds; a well-developed mature hardground profile is developed at the Cretaceous-Danian boundary (the ''Maastrichtian hardground''). Rare marl laminae are recorded and a discrete marly chalk bed associated with an interval of finegrained skeletal chalk wackestones near the top of the Maastrichtian is recognised in both wells. Comparison between the two wells demonstrates that the m-scale laminated-bioturbated chalk cycles described from the Dan Field area are both stratigraphically and areally restricted; this has implications for both cyclostratigraphic correlation and reconstruction of depositional environments and Late Maastrichtian evolution of the Danish Central Graben. (au)

Study on Character of Micro-Canal Deposit and Its Significance in Petroleum Geology --Case study of Tuo-147-well in north zone of Dongying depression

Institute of Scientific and Technical Information of China (English)

吴李泉; 曹代勇; 刘里勤; 刘艳华

2003-01-01

Exploration on reservoir of glutenite segment in steep slope zone of half graben-like basin is one of the hot spot targets at present and in the future for new reservoirs; And the study of sediment character of sandy-conglomerate bodies is the keystone and also the difficult problem. Taking Tuo-147-well area in north zone of Dongying depression as an example, the micro-canal sedimentation was researched. The result shows that many micro-canals exist at the end of slope grain-flow in steep slope zone of half graben-like basin; The micro-canals grow at the end of subaqueous grain-flow deposited bodies of 3rd member of the Shahejie formation. The main condition of micro-canal formation is the slope angle less than 18° and a long suitable sedimentary slope. These micro-canals may communicate the reservoir of glutenite segment in steep slope zone and the hydrocarbon stratum as a bridge role. Therefore, it is significant in theory and practice for discovering a series of micro-canals at the end of slope grain-flow in steep slope zone of half graben-like basin.

Palynology of the middle jurassic lower graben sand formation of the U-1 well, Danish Central Trough

Energy Technology Data Exchange (ETDEWEB)

Hoelstad, T.

1986-01-01

Twenty-one sidewall core samples from the lower 56 metres of the Lower Graben Sand Formation in the U-1 well are described with respect to their kerogen content and microflora in order to gain a better understanding of the depositional environment and the age relations. Based on e.g. the inconsistent dinoflagellate cyst occurrences, marginal marine conditions are concluded. The dinoglagellate cyst Pareodinia prolongata, Acanthaulax senta, Scriniodinium crystallinum, Energlynia acollaris, Wanaea thysanota and Hystrichogonyaulax cladophora and the recovered playnomorph assemblage in general permit an age determination as follows: 21 m Collovian undifferentiated, 7.9 latest Middle Callovian - earliest Late Callovian, 6.1 m latest Late Callovian and 21 m latest Late Callovian. - earliest Early Oxfordian.

Individualismo y desconfianza en el trabajo asociativo de cadenas productivas de agroexportacion en el Valle del Mantaro, Junín, Perú

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William Rodríguez Giráldez

2014-12-01

Full Text Available Objetivos: Determinar el individualismo y desconfianza en el trabajo asociativo de cadenas productivas de agroexportación en el Valle del Mantaro. Métodos: Investigación descriptiva, no experimental, de alcance transeccional correlacional. Fueron encuestados 383 productores agrícolas de las provincias que comprenden el Valle del Mantaro: Huancayo, Concepción, Jauja y Chupaca. Se utilizaron los estadísticos descriptivos, distribución de frecuencias, tablas de contingencia, y chi cuadrado para prueba de hipótesis. Resultados: En la dimensión individualismo: 72,23 % de productores manifestaron una actitud positiva hacia cadenas productivas; 87,2 % estimaron importante participar en reuniones; 88,5 % consideraron importante la capacitación en asociatividad y 86,2 % gustan trabajar conjuntamente con vecinos. Se deduce que el 83,53 % de ellos no tienen el rasgo de individualismo; por tanto, solo el 16,47 % tienen este rasgo y no influye negativamente en el trabajo asociativo en el Valle del Mantaro. En la dimensión desconfianza: 52 % de productores agrícolas manifestaron buena comunicación en la cadena productiva; 40 % aportaron entre 50 % y 100 % de costos de producción; 56 % podrían aportar entre 50 % y 100 % de costos de producción; 60 % señalaron que confían en empresas articuladoras y 60 % confían en colegas productores. Se deduce que, 53,6 % de estos productores no poseen el rasgo de desconfianza; mientras que 46,4 % si los tienen. Conclusiones: Solo 16,47 % de productores agrícolas tienen rasgos de individualismo y no influye negativamente en el trabajo asociativo; 46,4 % de estos productores tienen el rasgo de desconfianza y este valor sí influye negativamente en el trabajo asociativo en el valle.

Half-and-Half Palatoplasty.

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Han, Hyun Ho; Kang, In Sook; Rhie, Jong Won

2014-08-01

A 14-month-old child was diagnosed with a Veau Class II cleft palate. Von Langenbeck palatoplasty was performed for the right palate, and V-Y pushback palatoplasty was performed for the left palate. The child did not have a special problem during the surgery, and the authors were able to elongate the cleft by 10 mm. Contrary to preoperative concerns regarding the hybrid use of palatoplasties, the uvula and midline incisions remained balanced in the middle. The authors named this combination method "half-and-half palatoplasty" and plan to conduct a long-term follow up study as a potential solution that minimizes the complications of palatoplasty.

Descriptions and records of Cladiopsocidae and Dolabellopsocidae (Insecta: Psocodea: 'Psocoptera') from Valle del Cauca and National Natural Park Gorgona, Colombia.

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Calderón-Martínez, Nadia R; González-Obando, Ranulfo; Aldrete, Alfonso N García

2014-11-28

The results of a survey on the species diversity of the families Cladiopsocidae and Dolabellopsocidae (Psocodea: 'Psocoptera': Psocomorpha: Epipsocetae) in Valle del Cauca and in the National Natural Park (NNP) Gorgona, Colombia, are presented. The specimens studied were collected in the context of two scientific projects, in which 12 species in the two families were identified, five in Cladiopsocidae and seven in Dolabellopsocidae. In the first family, Cladiopsocus presented a new record in the country and four new species; in the latter, two genera were identified, Dolabellopsocus, with three new species and two new records, and Isthmopsocus, with two new species. This study presents the description of the nine new species from Valle del Cauca and NNP Gorgona, the new records for Colombia and identification keys to the neotropical species of both families.

Hurst analysis of seismicity in Corinth rift and Mygdonia graben (Greece)

International Nuclear Information System (INIS)

Gkarlaouni, Charikleia; Lasocki, Stanislaw; Papadimitriou, Eleftheria; George, Tsaklidis

2017-01-01

Highlights: • Long-term memory properties of seismicity are investigated using R/S analysis. • Small and moderate earthquake interevent times exhibit strong interdependence. • Strong earthquake occurrence indicates a memoryless process. • Seismicity variations in time are associated with Hurst temporal fluctuations. - Abstract: Temporal and spatial analysis of seismicity is performed via the Rescaled Range (R/S) analysis for revealing the hidden characteristics of long memory dependence and clustering between earthquakes. The analysis is applied in two seismogenic units belonging to the extensional Aegean back-arc region, namely the Corinth rift and the Mygdonian graben. The Hurst exponent estimations were used for the interpretation of earthquake collective properties, regarding magnitude, interevent time and interevent epicentral distance for consecutive events. Additional stochastic tools were then engaged for the validation of the results. Τhe analysis outcome is a significant long memory content in the seismic process of both areas, especially for the interevent time of recent micro seismicity and moderate earthquakes in the last decades. This property is not ascertained for the strong (M ≥ 6.0) historical earthquakes indicating that stronger events are rather independent, whereas the weaker ones may be primary carriers of persistence in the seismogenesis process.

Geochemistry of thermal fluids in NW Honduras: New perspectives for exploitation of geothermal areas in the southern Sula graben

Science.gov (United States)

Capaccioni, Bruno; Franco, Tassi; Alberto, Renzulli; Orlando, Vaselli; Marco, Menichetti; Salvatore, Inguaggiato

2014-06-01

The results of a geochemical survey on thermal waters and, for the first time for this site, gas discharges in five geothermal sites (Azacualpa "La Cueva", Río Ulua, Río Gualcarque, El Olivar and Laguna de Agua Caliente) in NW Honduras are here presented and discussed. El Olivar and Laguna de Agua Caliente, in the southern part of the Sula graben are very close to a Quaternary basaltic field, whereas Azacualpa "La Cueva", Río Ulua and Río Gualcarque, located to the southwest of the Yojoa Lake, direcly emerge from the Cretaceous limestone deposits. The measured temperatures range between 37.5 and 104.8 °C. "Mature", alkaline, Na-SO4 thermal waters discharge from Azacualpa "La Cueva", while those from El Olivar and Laguna de Agua Caliente are "immature" and show a Na-HCO3 composition. Chemical equilibria of waters and gases from the Azacualpa "La Cueva" thermal springs indicate temperatures ranging from 150 to 200 °C. Conversely, gas discharges from El Olivar and Laguna de Agua Caliente have attained a partial chemical equilibrium in the liquid phase at slightly higher temperatures (200-250 °C), although gas-gas faster reactions involving CO seem to be adjusted in an isothermally separated vapor phase. Unlike Azacualpa, SiO2 geothermometer at El Olivar and Laguna de Agua Caliente indicates equilibrium temperatures for the liquid phase much lower than those calculated for the gas phase (≤ 120 °C). We conclude that thermal waters from the Azacualpa area likely represent the direct emergence of a water dominated reservoir having temperatures ≤ 150-200 °C. By contrast, at El Olivar and Laguna de Agua Caliente hot springs are supplied by a boiling shallow aquifer fed by a vapor phase rising from a steam-dominated zone. The above geochemical model is consistent with a geothermal reservoir hosted within the Cretaceous carbonate sequences of the Yojoa Group in the whole investigated sites. The reservoir extensively crops out in the Azacualpa area whereas the

Assessment of Groundwater Supply Impacts for a Mine Site in Western Turkey

Science.gov (United States)

Agartan, E.; Yazicigil, H.

2010-12-01

A nickel mine located in Turgutlu town in Western Turkey requires 135 L/s of water for the mining processes. The initial studies pointed out that part of the supply will be met by pumping water from the Turgutlu-Salihli aquifer system. The purpose of this study is to assess the impacts associated with meeting groundwater supply requirements for the mine. Scope of the study involved development of the groundwater flow model of the Turgutlu-Salihli aquifer system, determination of the alternative groundwater pumping scenarios, assessment of the impacts associated with each scenario and selection of the most feasible scenario in the aspect of environmental and technical factors. Turgutlu town is located in one of the most tectonically active areas in Turkey which is characterized by an E-W trending Gediz Graben formed as a result of N-S directed extension. Gediz River as a major surface water resource in the study area flows from east to west, passes through Gediz Graben and is connected to the Turgutlu-Salihli aquifer system. Quaternary deposits and Neogene rocks, showing better aquifer properties than the other formations of the Gediz Graben, form the Turgutlu-Salihli aquifer system. Quaternary deposits form the principal aquifer, and Neogene rocks form the secondary aquifer in the study area. Therefore, a two layered groundwater flow model of the Turgutlu-Salihli aquifer system was established using MODFLOW. The model was calibrated under steady state conditions assuming that the conditions in 1991 prior to the significant development represented a pseudo-steady state in the aquifer system. Calibration was carried out for hydraulic conductivity, recharge and boundary conditions. To get today’s groundwater levels, wells being drilled after 1991 were added to the model. In the scope of this study, two potential scenarios were considered, and their effects on the aquifer systems were evaluated. The locations of the scenario wells were determined so that they will

Système d'information agricole dans la vallée de Huaral, au Pérou ...

International Development Research Centre (IDRC) Digital Library (Canada)

Evaluación del componente "Investigación aplicativa" del proyecto "Sistema de Información Agraria - SIA, a favor de los Pequeños Agricultores del Valle de Huaral" : el uso de "smartphones" en el medio rural como herramienta para el acceso a la... Téléchargez le PDF. Rapports. Sistema de información agraria : SIA del ...

Traces of the Book Vatican Policy in the Manuscript File of Ramón del Valle-Inclán

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Amparo de Juan Bolufer

2017-01-01

Full Text Available In various interviews done in 1933 Valle-Inclán said he was preparing a book for the historic series El Ruedo Ibérico that would explore the influence of the Vatican in Spanish politics. This article seeks to examine the traces of this narrative plan that have been preserved in the manuscript file belonging to the Valle-Inclán Alsina family, because we know that the writer continued to work on this historical project until his death. After examining the indirect documentation located primarily in the periodical press which bears witness to the process of writing this never published story, we will describe the unknown plans of structure and the drafts of work that are part of this creation file and that allow us to perceive the plot lines as well as the fundamental features of characterization for the prominent protagonists in this incomplete project.

Studying Disability and Disability Studies: Shifting Paradigms of LD -- A Synthesis of Responses to Reid and Valle

Science.gov (United States)

Connor, David J.

2005-01-01

In this article, I discuss the 11 diverse responses to Reid and Valle's work on the discursive practice of learning disabilities (LD), implications for instruction, and parent-school relations. I highlight key ideas from each article and then focus on three common areas of interest shared by most respondents: the unacceptable status quo of…

The Nile valley of Egypt: A major active graben that magnifies seismic waves

International Nuclear Information System (INIS)

EI-Sayed, A.; Vaccari, F.; Panza, G.F.

2002-08-01

The Nile valley and the Nile delta are part of the active rift that is probably connected with the Red Sea tectonism. This zone is characterized by small to moderate size earthquakes that have caused extremely severe damage to recent and historical constructions. The most vulnerable area along the Nile valley is the one of Cairo-Faiyoum. Small local and large distant earthquakes could be a source of huge socio-economic damage in this area. The loose soft alluvial sediments of the Nile Canyon are the main factors behind this potential damage because they may greatly amplify the ground motion, as demonstrated by strong ground motion modelling. The largest amplification is generally concentrated along the edges of the graben and occurs at frequencies between 1 Hz and 2 Hz. This may explain the huge damage caused by distant earthquakes during recent and historical times. The distribution of intensity values during the events of 1926 and 1992 is well correlated with the modelled spatial distribution of the spectral amplification. (author)

SEROPREVALENCIA Y SEROTIPIFICACIÓN DE LEPTOSPIROSIS CANINA EN EL MUNICIPIO DE BUENAVENTURA (VALLE DEL CAUCA)

OpenAIRE

Romero Peñuela, Marlyn Hellen; Astudillo Hernández, Myriam; Quintero Martínez, Mauricio Elías

2009-01-01

El presente estudio tuvo como objetivo verificar la infección con serovares de Leptospira spp. en caninos con propietario en Buenaventura, Valle del Cauca, Colombia. Las muestras de suero fueron tomadas de 100 caninos y fueron probadas con los serogrupos de Leptospira interrogans: Bataviae, Mini, Autumnalis, Canicola, Shermani, Icterohaemorrhagiae, Cynopteri, Australis, Celledonis, Grippotyphosa, Hebdomadis, Javanica, Manhao, Pomona, Pyrogenes, Sejroe, Tarassovi y Ballum, usando la técnica de...

Neogene amphibians and reptiles (Caudata, Anura, Gekkota, Lacertilia, and Testudines) from the south of Western Siberia, Russia, and Northeastern Kazakhstan.

Science.gov (United States)

Vasilyan, Davit; Zazhigin, Vladimir S; Böhme, Madelaine

2017-01-01

The present-day amphibian and reptile fauna of Western Siberia are the least diverse of the Palaearctic Realm, as a consequence of the unfavourable climatic conditions that predominate in this region. The origin and emergence of these herpetofaunal groups are poorly understood. Aside from the better-explored European Neogene localities yielding amphibian and reptile fossil remains, the Neogene herpetofauna of Western Asia is understudied. The few available data need critical reviews and new interpretations, taking into account the more recent records of the European herpetofauna. The comparison of this previous data with that of European fossil records would provide data on palaeobiogeographic affiliations of the region as well as on the origin and emergence of the present-day fauna of Western Siberia. An overview of the earliest occurrences of certain amphibian lineages is still needed. In addition, studies that address such knowledge gaps can be useful for molecular biologists in their calibration of molecular clocks. In this study, we considered critically reviewed available data from amphibian and reptile fauna from over 40 Western Siberian, Russian and Northeastern Kazakhstan localities, ranging from the Middle Miocene to Early Pleistocene. Herein, we provided new interpretations that arose from our assessment of the previously published and new data. More than 50 amphibians and reptile taxa were identified belonging to families Hynobiidae, Cryptobranchidae, Salamandridae, Palaeobatrachidae, Bombinatoridae, Pelobatidae, Hylidae, Bufonidae, Ranidae, Gekkonidae, Lacertidae, and Emydidae. Palaeobiogeographic analyses were performed for these groups and palaeoprecipitation values were estimated for 12 localities, using the bioclimatic analysis of herpetofaunal assemblages. The Neogene assemblage of Western Siberia was found to be dominated by groups of European affinities, such as Palaeobatrachidae, Bombina, Hyla , Bufo bufo , and a small part of this assemblage

Pueblos, rituales y condiciones de vida prehispánicas en el Valle del Cauca

OpenAIRE

Rodríguez Cuenca, José Vicente

2005-01-01

El Valle del Cauca estuvo habitado por diversos pueblos que desarrollaron ingeniosas estrategias adaptativas con el propósito de mantener el equilibrio homeostasis entre la producción de recursos y su consumo. Los sacrificios humanos, las cabezas trofeo, el canibalismo ritual, los festejos asociados a las cosechas, los rituales funerarios, el sostenimiento de tierras de nadie en áreas fronterizas, los mismos combates organizados entre grupos rivales, la exogamia, la reprocidad y el intercambi...

Rubén Darío y Valle-Inclán Diálogo intercultural // Rubén Darío and Valle-Inclán: An intercultural dialogue

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José María Paz Gago

2016-12-01

Full Text Available The author discusses the relationship between two writers, representatives of literature at the turn of the twentieth century, seen as a dialogue both human and intercontinental. The Spaniard Valle-Inclán and the Nicaraguan Darío developed the inheritance of late Romanticism and decadence, they were formed during the epoch of symbolism and French parnasism, and participated in the constitution of Hispanic modernism. The essay offers a commentary on several texts they dedicated to each other, which create an authentic intercultural dialogue.

Neogene Uplift and Magmatism of Anatolia: New Insights from Drainage Analysis and Basalt Geochemistry

Science.gov (United States)

McNab, F.; Ball, P.; Hoggard, M.; White, N.

2017-12-01

The origin of Anatolia's high elevation and low relief plateaux has been the subject of much recent debate. Marine sedimentary rocks distributed across Central and Eastern Anatolia require significant regional uplift in Neogene times. This uplift cannot be explained by the present-day pattern of crustal deformation which, particularly across Central and Western Anatolia, is dominanted by strike-slip and extensional faulting. Positive long wavelength free-air gravity anomalies combined with slow upper mantle seismic wave speeds suggest that the sub-lithospheric mantle provides substantial topographic support. A range of geodynamic processes have been invoked, including complex slab fragmentation and lithospheric delamination. The temporal and spatial evolution of the Anatolian landscape should be recorded by drainage networks. Indeed, major catchments contain prominent knickzones with heights of hundreds of meters and length scales of several hundred kilometers. The stream power formulation for fluvial erosion permits these knickzones to be interpreted in terms of uplift history along a river's length. Here, we jointly invert an inventory of 1,844 river profiles to determine a spatial and temporal uplift rate history. When calibrated against independent observations of uplift rate, the resultant history provides significant new constraints for the evolution of Anatolian topography. In our model, the bulk of this topography appears to grow in Neogene times. Uplift initiates in Eastern Anatolia and propagates westward at uplift rates of up to 0.5 mm/yr. Coeval with this phase of uplift, abundant basaltic magmatism has occurred throughout Anatolia. We have compiled an extensive database of published geochemical analyses. Using this database, we analyse spatial and temporal patterns of basaltic compositions to discriminate between different modes of melt generation. Two independent techniques for estimating asthenospheric potential temperatures from the compositions of

Structural heritage, reactivation and distribution of fault and fracture network in a rifting context: Case study of the western shoulder of the Upper Rhine Graben

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Bertrand, Lionel; Jusseaume, Jessie; Géraud, Yves; Diraison, Marc; Damy, Pierre-Clément; Navelot, Vivien; Haffen, Sébastien

2018-03-01

In fractured reservoirs in the basement of extensional basins, fault and fracture parameters like density, spacing and length distribution are key properties for modelling and prediction of reservoir properties and fluids flow. As only large faults are detectable using basin-scale geophysical investigations, these fine-scale parameters need to be inferred from faults and fractures in analogous rocks at the outcrop. In this study, we use the western shoulder of the Upper Rhine Graben as an outcropping analogue of several deep borehole projects in the basement of the graben. Geological regional data, DTM (Digital Terrain Model) mapping and outcrop studies with scanlines are used to determine the spatial arrangement of the faults from the regional to the reservoir scale. The data shows that: 1) The fault network can be hierarchized in three different orders of scale and structural blocks with a characteristic structuration. This is consistent with other basement rocks studies in other rifting system allowing the extrapolation of the important parameters for modelling. 2) In the structural blocks, the fracture network linked to the faults is linked to the interplay between rock facies variation linked to the rock emplacement and the rifting event.

Receiver-operating characteristic curves for somatic cell scores and California mastitis test in Valle del Be lice dairy sheep

NARCIS (Netherlands)

Riggio, V.; Pesce, L.L.; Morreale, S.; Portolano, B.

2013-01-01

Using receiver-operating characteristic (ROC) curve methodology this study was designed to assess the diagnostic effectiveness of somatic cell count (SCC) and the California mastitis test (CMT) in Valle del Belice sheep, and to propose and evaluate threshold values for those tests that would

Structural observations from the Canavese Fault west of Valle d'Ossola (Piemonte) and some time constraints

Science.gov (United States)

Pleuger, Jan; Mancktelow, Neil

2010-05-01

The Canavese Fault (CF) is the SW part of the most important fault system in the Alps, the Periadriatic Fault. The CF has a complex kinematic history involving an older stage of NW-side-up faulting and a younger stage of SE-side-up plus dextral faulting in the area of Valle d'Ossola (Schmid et al. 1987). There, shearing occurred under greenschist-facies conditions and the fault is a c. 1 km thick mylonite zone. Toward SW, faulting took place under progressively lower temperatures and the volume of rocks affected by S-side-up plus dextral shearing becomes larger at the expense of the N-side-up mylonites. S of Valle Sesia, brittle fault rocks dominate over mylonites. Still further SW, close to the Serra d'Ivrea, the CF splits into two branches, the Internal Canavese Fault (ICF) and the External Canavese Fault (ECF). S-side-up plus dextral faulting is localised along the ICF while the observed displacement senses at the ECF are mostly, though not always, N-side-up and sinistral. Age constraints for faulting along the CF are mostly derived from absolute ages of magmatic rocks exposed alongside or within the fault. In the section around Biella, NW-side-up faulting cannot have lasted longer than until 31±2 Ma (Scheuring et al. 1974) because this is the age of andesites overlying the basement of the Penninic Sesia Zone. However, some additional uplift of the Sesia Zone with respect to the South Alpine Ivrea Zone was accommodated by down-to-the-SE tilting of the Sesia zone around a roughly NNE-SSW-trending subhorizontal axis which is evidenced by palaeomagnetic data (Lanza 1977). As a result of that, the Early Oligocene Biella Pluton (c. 31 Ma, Romer et al. 1996) today occupies a similar altitude level as the andesites of the same age. Post-31-Ma uplift of the Ivrea Zone with respect to the andesites is evidenced by the Early Oligocene (29-33 Ma, Carraro & Ferrara 1968) Miagliano Pluton which is hosted by the Ivrea Zone rocks and exposed at the present topographic surface

Fraccionamiento de nitrógeno en frijol ( phaseolus vulgaris l. en el valle de san juan

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Juan Cedano

2000-01-01

Full Text Available Fraccionamiento de nitrógeno en frijol (Phaseolus vulgaris L. en el valle de San Juan. Se realizó un estudio para determinar el efecto del fraccionamiento de la fertilización nitrogenada y el momento adecuado para la aplicación de nitrógeno en el cultivo de frijol (Phaseolus vulgaris L. en cinco localidades del Valle de San Juan, R. D. Los experimentos fueron establecidos del 5 al 14 de noviembre (1997 , se utilizó un diseño de bloques completamente al azar y nueve tratamientos en cada localidad, encontrándose que en los terrenos con altos niveles de nitrógeno no hubo respuesta a la aplicación de nitrógeno ni al fraccionamiento de este nutrimento; mientras que en los suelos con deficiencia en nitrógeno si hubo respuesta a la fertilización nitrogenada encontrándose diferencia estadística significativa a la aplicación y al momento de aplicación del fertilizante. Entre las localidades hubo diferencia estadística significativa (P>0.05, mientras que no se encontró interacción entre los tratamientos y las localidades

Determinantes del trabajo infantil y la escolaridad: el caso del Valle del Cauca en Colombia

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Sebastián Urueña Abadía

2009-10-01

Full Text Available Colombia, al igual que la mayoría de países latinoamericanos, consciente de las repercusiones sociales y económicas negativas del trabajo infantil, se ha comprometido en la lucha por la erradicación de este fenómeno. Prueba de ello es la ratificación por parte del gobierno colombiano en el año 2007, del Convenio 182 de la OIT sobre la Prohibición de las Peores Formas de Trabajo Infantil y la Acción Inmediata para su Eliminación. En el plano regional, como parte del Plan de Desarrollo del Departamento del Valle del Cauca 2008-2011, se está implementando actualmente una estrategia territorial de erradicación del trabajo infantil en sus 42 municipios. Considerando este panorama, este trabajo indaga cuáles son los determinantes del trabajo infantil y la escolaridad en el departamento del Valle a partir de los datos de la Encuesta Nacional de Calidad de Vida del año 2003. Para el análisis se emplea un modelo econométrico Probit Bivariado, que permite el estudio conjunto e interrelacionado de decisiones diferentes, en este caso la asistencia escolar y el trabajo.

Materials for the study of the bronze age in the valley of the Vinalopo (Alicante | Materiales para el estudio de la Edad del Bronce en el Valle Medio del Vinalopó (Alicante | Materiales para el estudio de la Edad del Bronce en el Valle Medio del Vinalopó (Alicante

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Juan Francisco Navarro Mederos

1982-12-01

Full Text Available Se presenta un grupo de poblados del Bronce en el Valle Medio del Vinalopó, provincia de Alicante, y los materiales procedentes de ellos y conservados en colecciones privadas. Su conocimiento permite incluir esta comarca en la cultura del Bronce Valenciano —aunque manteniendo una cierta personalidad— y aventurar hipótesis sobre la dinámica de la Edad del Bronce a lo largo de la cuenca del Vinalopó, sus contactos exteriores, las fronteras con el mundo argárico e intentar ordenarlos cronológicamente en base a un esquema propuesto para la globalidad del Bronce Valenciano. | L'article offre l'étude d'un groupe de sites de l'âge du Bronze dans la vallée du Vinalopó et des matériaux archéologiques conservés dans des collections privées. Des resultats de cet étude on peut inférer l'appartenance de cette zone a la civilisation du Bronze Valenciano, tout en conservant des traits individuants, et aussi tenter d'expliquer la dynamique de l'âge du Bronze au long de la vallée du Vinalopó, ses rapports extérieurs et la frontière avec la civilisation de l'Argar. On donne également une tentative de chronologie fondee sur un schéma global pour le Bronze Valenciano.

Neogene sea surface temperature reconstructions from the Southern McMurdo Sound and the McMurdo Ice Shelf (ANDRILL Program, Antarctica)

Science.gov (United States)

Sangiorgi, Francesca; Willmott, Veronica; Kim, Jung-Hyun; Schouten, Stefan; Brinkhuis, Henk; Sinninghe Damsté, Jaap S.; Florindo, Fabio; Harwood, David; Naish, Tim; Powell, Ross

2010-05-01

During the austral summers 2006 and 2007 the ANtarctic DRILLing Program (ANDRILL) drilled two cores, each recovering more than 1000m of sediment from below the McMurdo Ice-Shelf (MIS, AND-1B), and sea-ice in Southern McMurdo Sound (SMS, AND-2A), respectively, revealing new information about Neogene Antarctic cryosphere evolution. Core AND-1B was drilled in a more distal location than core AND-2A. With the aim of obtaining important information for the understanding of the history of Antarctic climate and environment during selected interval of the Neogene, we applied novel organic geochemistry proxies such as TEX86 (Tetra Ether IndeX of lipids with 86 carbon atoms) using a new calibration equation specifically developed for polar areas and based on 116 surface sediment samples collected from polar oceans (Kim et al., subm.), and BIT (Branched and Isoprenoid Tetraether), to derive absolute (sea surface) temperature values and to evaluate the relative contribution of soil organic matter versus marine organic matter, respectively. We will present the state-of-the-art of the methodology applied, discussing its advantages and limitations, and the results so far obtained from the analysis of 60 samples from core AND-2A covering the Miocene Climatic Optimum (and the Mid-late Miocene transition) and of 20 pilot samples from core AND-1B covering the late Pliocene.

Patrimonio cultural prehispánico y peligro geodinámico en el valle del Huatanay - Cusco

Directory of Open Access Journals (Sweden)

2005-01-01

Full Text Available Patrimoine culturel pré-hispanique et aléa géodynamique dans la vallée du Huatanay, Cusco Résumé: Parmi les nombreux sites archéologiques pré-hispaniques de la vallée de Huatanay, Cusco, plusieurs sont menacés ou en train d’être détruits par des phénomènes de géodynamique externe (glissements de terrain, éboulements, alluvions torrentielles, karstification et érosion. La plupart de ces processus ont une dynamique lente, mais plusieurs d’entre eux montrent des signes d’accélération, due à leur dynamique propre ou sont aggravés par des interventions humaines : le manque de maintenance, la déprédation, les activités agricoles et forestières inadéquates, l’urbanisation et le tourisme non contrôlés. De los numerosos conjuntos arqueológicos prehispánicos existentes en el valle del Huatanay, Cusco, varios se encuentran amenazados o están siendo destruidos por fenómenos de geodinámica externa (deslizamientos, derrumbes, lavas torrenciales y karstificación y erosión. La mayoría de estos procesos son de carácter lento, pero muchos muestran signos de aceleración debido a su dinámica natural o por intervenciones humanas: la falta de mantenimiento, la depredación, las actividades agropecuarias y forestales inapropiadas, la urbanización y el turismo no controlados Pre-hispanic archeological heritage and geodynamic hazard in the valley of Huatanay - Cuzco Abstract: Of the numerous Prehispanic archaeological complexes located in the Huatanay Valley Cusco, several are threatened or are being destroyed by external geodynamics phenomena (landslides, rock falls, lava flows, karstification and erosion. Most of these processes are slow, but many of them show signs of acceleration, due to their natural dynamics or by humain intervention: lack of maintenance, depredation, inappropriate agricultural and forestry activities, and uncontrolled urbanization and tourism.

Mangrove associated lignite beds of Malvan, Konkan: Evidence for higher sea-level during the Late Tertiary (Neogene) along the west coast of India

Energy Technology Data Exchange (ETDEWEB)

Kumaran, K.P.N.; Shindikar, M.; Limaye, R.B. [Agharkar Research Inst., Pune (India)

2004-01-25

Fossil pneumatophores (breathing roots) of Avicennia are recovered and reported from the lignite beds exposed in Kolamb well-section near Malvan, Konkan area of western Maharashtra. The accrued palynoflora is dominated by mangroves (Avicennia, Aegialitis, Excoecaria, Rhizophora and Sonneratia). The spores of mangrove fern (Acrostichum aureum) an estuarine fungus Cirrenalia indicate that these lignites are autochthonous and deposited in a near-shore environment. Presence of foraminiferal linings (= microforaminifera), dinoflagellate cysts, a few calcareous nannofossils and scolecodonts is an irrefutable proof of marine and brackish water influence during the deposition of lignites under intertidal/tidal swampy condition (mangrove influenced) with fair input from freshwater swamps and hinterland. Freshwater-related forms, viz. Ceratopteris thalictroides, Nymphaeaceae, Ctenolophonaceae and hinterland taxa (Cullenia/Durio) of Bombacaceae along with abundance of microthyriaceous fungi in the palynoflora imply a warm humid tropical climate with high precipitation during the depositional period. The presence of Ctenolophon englerianus (= Ctenolophonidites costatus) in Kolamb lignites suggests the Late Neogene (Late Miocene-Early Pliocene) age. The occurrence of pneumatophores and associated lignite deposits about 37 m above the present mean sea-level, and much inland, clearly indicates the higher sea-level strand during Late Neogene along the west coast of India.

Paleomagnetic results of Neogene strata in Eastern Vietnam and their paleogeographic Implications

Science.gov (United States)

Weiwei, C.; Zhao, X.; Liu, Z.; Dong Pha, P.

2017-12-01

Neogene paleomagnetic data from the Vietnam, southeastern margin of the Indochina Block, are essential to reconstruct post-collisional paleogeography. This is key to understanding the evolution of the western South China Sea and verifying the model of extrusion tectonic. Mid-Miocene siltstone of the Song Ba Formation and Pliocene basalt were sampled from Phu Tue area, eastern Vietnam. Paleomagnetic samples were collected using a gasoline-powered drill and a magnetic compass mounted on an orienting device. We corrected for the effect of local magnetic anomalies on magnetic orientation by taking solar azimuths using a sun compass. For most samples, the discrepancy between the two compass readings is within 3°. Remanent magnetization measurements were carried out with 2G-755-4K cryogenic magnetometers, installed in the Plaleomagnetism Laboratory, Tongji University, Shanghai. All the instruments are located in a shielded room with residual fields less than 200 nT. The anisotropy of magnetic susceptibility (AMS) results of four siltstone sites (sites 2, 6, 9, 10) indicate the siltstone preserve a normal sedimentary magnetic fabric. The other sites of the AMS (including basalt sites) show that the directions of K1, K2, K3 are scattered without any regulation. The thermal demagnetization and AF demagnetization were performed on specimens and stepwise demagnetization up to 600°C or 150 mT. ChRM directions were determined for all the specimens using principal component analysis. The directions obtained from Neogene rocks are far from the present geomagnetic field (PGF) and include antipodal dual polarities, suggesting a primary origin. A visible fluctuation in paleomagnetic direction from one site to another is evident from the results. Shallow inclination are obtained from most samples which range of 7.4° to 21.5°. The siltstone declination range of 16.8° to 34.5° while the basalt declination rang of 178.3° to 335.0°. This wide range of direction fluctuation

Stratigraphy and erosional landforms of layered deposits in Valles Marineris, Mars

Science.gov (United States)

Komatsu, G.; Geissler, P. E.; Strom, R. G.; Singer, R. B.

1993-01-01

Satellite imagery is used to identify stratigraphy and erosional landforms of 13 layered deposits in the Valles Marineris region of Mars (occurring, specifically, in Gangis, Juventae, Hebes, Ophir-Candor, Melas, and Capri-Eos Chasmata), based on albedo and erosional styles. Results of stratigraphic correlations show that the stratigraphy of layered deposits in the Hebes, Juventae, and Gangis Chasmata are not well correlated, indicating that at least these chasmata had isolated depositional environments resulting in different stratigraphic sequences. On the other hand, the layered deposits in Ophir-Candor and Melas Chasmata appear to have been connected in each chasma. Some of the layered deposits display complexities which indicate changes in space and time in the dominant source materials.

Seismotectonics of Western Turkey: A Synthesis of Source Parameters and Rupture Histories of Recent Earthquakes

Science.gov (United States)

Taymaz, T.; Tan, O.; Yolsal, S.

2004-12-01

The Aegean region, including western Turkey and Greece, is indeed one of the most seismically active and rapidly deforming continental domains in the Earth. The wide range of deformational processes occurring in this region means that the eastern Mediterranean provides a unique opportunity to improve our understanding of the complex kinematics of continental collision, including strike-slip faulting and crustal extension, as well as associated seismicity and volcanism. The tectonic evolution of the Eastern Mediterranean region is dominated by effects of subduction along the Hellenic (Aegean) arc and of continental collision in eastern Anatolia and the Caucasus. Northward subduction of the African plate beneath western Anatolia and the Aegean region is causing crustal extension in the overlying Aegean province. The interplay between dynamic effects of the relative motions of adjoining plates thus controls large-scale crustal deformation and the associated earthquake activity in Turkey. The Aegean region has been subject to extension since Miocene time, and this extension has left a pronounced expression in the present-day topography. It is further widely accepted that the rapid extension observed in western Turkey is mainly accommodated by large active normal faults that control the geomorphology which is dominated by a series of E-W trending normal-fault-bounded horst and graben structures; the N-S extension inferred from these structures is consistent with regional earthquake focal mechanisms. The E-W trending Menderes graben, the NE-SW trending Burdur, Acigol and Baklan, and NW-SE trending Dinar and Sultandag-Aksehir basins all bounded by large faults form a system of half-graben whose orientation is evident in both the topography and the tilting of Neogene sediments adjacent to them. We have studied source mechanisms and rupture histories of ˜20 earthquakes using body-waveform modelling, and have compared the shapes and amplitudes of teleseismic long-period P

Los contratos de producción en el noreste de México: El valle de Mexicali a fines de la década de los ochenta

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Alejandra Stamatis Maldonado

1993-01-01

Full Text Available El objetivo del presente trabajo es analizar la presencia de contratos de producción entre los productores de hortalizas de exportación en el valle de Mexicali y el capital estadounidense. A partir de una caracterización de los productores de hortalizas en el valle de Mexicali, se describe la forma básica que asumen las relaciones de financiamiento y de comercialización con las compañías distribuidoras, y se analizan esas relaciones en el contexto de la producción de hortalizas de exportación en el noroeste de México

The Neogene molasse deposits of the Zagros Mountains in central Dezful Embayment: facies, sedimentary environments and controls

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Ali Hossein Jalilian

2016-03-01

Full Text Available The upper part of Neogene sequence of the Zagros Mountains consists of a clastic succession which is identified as Aghajari and Bakhtyari formations. The sequence is an excellent example of synorogenic sedimentation or molasse deposited in northern portion of the Zagros foreland basin. Sedimentological analysis of an outcrop section representing Miocene-Pliocene sediments in central Dezful Embayment resulted in recognizing 9 lithofacies and 4 architectural elements. These lithofacies include conglometate (Gt, Gh, Gmm, sandstone (Sp, Sh, Sr, St and mudstone (Fm, Fl that were deposited in meandering stream, braided river and alluvial fan environments. Paleocurrent analysis of cross-beds, channels and asymmetric ripple marks indicate that these Neogene clastics were mainly drived from Cretaceous to Paleogene highlands in the Zagros Mountains on the north. This stratigraphic record is coarsening-upward and formed by a regressive depositional megacycle under arid climate. Facies and depositional history analysis show that sedimentation of the Zagros molasse was primarily controlled by base-level changes rather than catchment lithology or climate. The sedimentary record of this regressive megacycle reveales the base-level was constantly falling down on one hand and the provenance was uplifting on the other hand. Tectonic activities and Zagros Mountains rising in the Late Miocene resulted in deposition of fining-upward point-bar and floodplain sequences of the Aghajari Formation in low-gradient meandering streams. The Lahbari Member of the Aghajari Formation represents deposition in braided rivers that composed predominantly of flood-plain deposits in the Early Pliocene. Finally, the sedimentary cycle of the Zagros molasse deposits terminated with massive conglomerates of the Bakhtyari Formation deposited in large alluvial fans near the source area.

Emplacement and erosive effects of the south Kasei Valles lava on Mars

Science.gov (United States)

Dundas, Colin M.; Keszthelyi, Laszlo P.

2014-01-01

Although it has generally been accepted that the Martian outflow channels were carved by floods of water, observations of large channels on Venus and Mercury demonstrate that lava flows can cause substantial erosion. Recent observations of large lava flows within outflow channels on Mars have revived discussion of the hypothesis that the Martian channels are also produced by lava. An excellent example is found in south Kasei Valles (SKV), where the most recent major event was emplacement of a large lava flow. Calculations using high-resolution Digital Terrain Models (DTMs) demonstrate that this flow was locally turbulent, similar to a previously described flood lava flow in Athabasca Valles. The modeled peak local flux of approximately 106 m3 s−1 was approximately an order of magnitude lower than that in Athabasca, which may be due to distance from the vent. Fluxes close to 107 m3 s−1 are estimated in some reaches but these values are probably records of local surges caused by a dam-breach event within the flow. The SKV lava was locally erosive and likely caused significant (kilometer-scale) headwall retreat at several cataracts with tens to hundreds of meters of relief. However, in other places the net effect of the flow was unambiguously aggradational, and these are more representative of most of the flow. The larger outflow channels have lengths of thousands of kilometers and incision of a kilometer or more. Therefore, lava flows comparable to the SKV flow did not carve the major Martian outflow channels, although the SKV flow was among the largest and highest-flux lava flows known in the Solar System.

Reinterpretation of the tectonics and formation of the Pernambuco Plateau Basin, NE Brazil.

Science.gov (United States)

Hoggett, Murray; Jones, Stephen M.; Dunkley Jones, Tom; Reston, Timothy; Barbosa, Antonio; Biondo, Vanessa; Mort, Haydon P.

2017-04-01

The continental margin from Alagoas to Natal represents arguably the most frontier region for exploration on the Brazillian margin. High quality seismic data was not collected in the region for many decades as it was believed that only a few kilometers of sediment existed, and thus there was no exploration potential. Here we present the results of work done as part of an IODP virtual site survey. The work has resulted in a total reinterpretation of the basin structure and tectonics, including finding sediment filled half grabens holding up to 8km thick stratigraphic sections. The two deepest grabens likely represent rift jumps during breakup, which may imply different age sediments in the different grabens. The basin is also found to contain a sizable salt accumulation, previously uninterpreted due to hard overlying carbonates hampering seismic imaging. This salt can be seen to have been highly mobile in the past, and has developed into kilometer scale diapirs flanked by typical rollover anticlines. For the first time we show the basin has all the elements needed for a working petroleum system, with the exception a source rock - which cannot be speculated on further as the basin is undrilled. However source rock sequences are present in the Alagoas basin to the south, and recent released seep data show evidence for both biogeneic and thermogenic seeps over the plateau basin, which could also signal source rock presence. We present seismic and potential fields data, including forward potential fields models and seismically derived crustal stretching and thinning estimates, to show that the half grabens terminate abruptly at the latitude of the Pernambuco Shear Zone, a major crustal scale Precambrian shear zone. Onshore boreholes, well away from the deep seismically imaged half grabens offshore, find crystalline basement to drop away rapidly across the shearzone, revealing a third graben to terminate at the shear zone. We interpret this as that the preexisting

Exportaciones del Valle del Cauca. Determinantes, comportamiento y prospectiva

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Dubán F. Peña Benítez

2007-01-01

Full Text Available Este trabajo centra su análisis en los determinantes de las exportaciones del Valle del Cauca en el periodo 1970 - 2004 y, en una predicción de corto y mediano plazo a través de un VAR y una función generalizada de impulso respuesta. Los hallazgos mostraron significancía de variables como el ingreso mundial (IM, el precio de los bienes exportables (TCR, los acuerdos comerciales (Aptdea y la dinámica de la oferta exportable (XV-1. La predicción para las exportaciones de la región estableció que la TCR tiene efectos positivos en el corto plazo, el ingreso mundial (IM impacta de forma positiva más en el largo que en el corto plazo y la variable acuerdos comerciales muestra importancia sólo de corto mas no de largo plazo.

Project Half Double

DEFF Research Database (Denmark)

Svejvig, Per; Gerstrøm, Anna; Frederiksen, Signe Hedeboe

The Half Double mission: Project Half Double has a clear mission. We want to succeed in finding a project methodology that can increase the success rate of our projects while increasing the development speed of new products and services. We are convinced that by doing so we can strengthen...... the competitiveness of Denmark and play an important role in the battle for jobs and future welfare. The overall goal is to deliver “Projects in half the time with double the impact” where projects in half the time should be understood as half the time to impact (benefit realization, effect is achieved......) and not as half the time for project execution. The Half Double project journey: It all began in May 2013 when we asked ourselves: How do we create a new and radical project paradigm that can create successful projects? Today we are a movement of hundreds of passionate project people, and it grows larger...

Neogene biostratigraphy and paleoenvironments of Enewetak Atoll, equatorial Pacific Ocean

Science.gov (United States)

Cronin, T. M.; Bybell, L.M.; Brouwers, E.M.; Gibson, T.G.; Margerum, R.; Poore, R.Z.

1991-01-01

Micropaleontologic analyses of Neogene sediments from Enewetak Atoll, Marshall Islands, provide data on the age of lagoonal deposits, stratigraphic disconformities and the paleoenvironmental and subsidence history of the atoll. Benthic foraminifers, planktic foraminifers, calcareous nannofossils and ostracodes were studied from six boreholes, the deepest penetrating 1605 feet below the lagoon floor into upper Oligocene strata. The Oligocene-Miocene boundary occurs at about 1200 ft below the lagoon floor. The early and middle Miocene is characterized by brief periods of deposition and numerous hiatuses. Ostracodes and benthic foraminifers indicate a shallow-marine reefal environment with occasional brackish water conditions. Upper Miocene and lower Pliocene deposits placed in calcareous nannofossil Zones NN9-15 and in planktic foraminifer Zones N16-19 contain species-rich benthic microfaunas which indicate alternating reefal and brackish water mangrove environments. The upper Pliocene contains at least two major depositional hiatuses that coincide with a major faunal turnover in benthic foraminiferal and ostracode assemblages. The Quaternary is characterized by benthic microfaunas similar to those of modern atoll lagoons and is punctuated by at least 11 disconformities which signify periods of low sea level. Atoll subsidence rates during the last 10 Ma averaged 30 to 40 m/m.y. ?? 1991 Elsevier Science Publishers B.V. All rights reserved.

Contributions of gravity and field data on the structural scheme updating of the Tellian domain and its foreland (Nefza-Bizerte region, northern Tunisia)

Science.gov (United States)

Essid, El Mabrouk; Kadri, Ali; Balti, Hadhemi; Gasmi, Mohamed; Zargouni, Fouad

2018-03-01

The Nefza-Bizerte region, eastern part of the Tunisian Alpine chain, covers the thrust sheets domain called the Tell and its Atlassic foreland. The deep structures under the Tellian thrust sheets are not enough explored. The structural interpretation of magmatic rocks, Triassic outcrops and the depressions are still a subject of discussion. In this work, we intend to investigate deep faults and their eventual role in magmatism and Triassic salt setting up and to explain the depression genesis. Analysis of the Bouguer anomaly map and its derivatives reveals the main gravity lineaments, organized in major NE- and NW-trending systems. The NE-trending system, dipping towards the NW, is the main component of the structural scheme and has controlled the tectonic evolution of this area. After the immobilization of the Tellian thrust sheets during the uppermost Langhian, the Tell and its Atlassic foreland were affected by the Tortonian compressive event with a NW-trending maximum horizontal stress. The reverse kinematics of the NE-trending deep-seated faults created at their front continental environments filled later by post-nappes Neogene deposits. After the early Pleistocene, a NNW-directed compressional stress regime deformed the post-nappes Neogene series and generated NW-trending grabens. This coexistence of compression-extension continues until present day.

Soft-Sediment Deformation Structures Interpreted as Seismites in the Kolankaya Formation, Denizli Basin (SW Turkey)

Science.gov (United States)

Topal, Savaş; Özkul, Mehmet

2014-01-01

The NW-trending Denizli basin of the SW Turkey is one of the neotectonic grabens in the Aegean extensional province. It is bounded by normal faults on both southern and northern margins. The basin is filled by Neogene and Quaternary terrestrial deposits. Late Miocene- Late Pliocene aged Kolankaya formation crops out along the NW trending Karakova uplift in the Denizli basin. It is a typical fluviolacustrine succession that thickens and coarsens upward, comprising poorly consolidated sand, gravelly sand, siltstone and marl. Various soft-sediment deformation structures occur in the formation, especially in fine- to medium grained sands, silts and marls: load structures, flame structures, clastic dikes (sand and gravely-sand dike), disturbed layers, laminated convolute beds, slumps and synsedimentary faulting. The deformation mechanism and driving force for the soft-sediment deformation are related essentially to gravitational instability, dewatering, liquefaction-liquidization, and brittle deformation. Field data and the wide lateral extent of the structures as well as regional geological data show that most of the deformation is related to seismicity and the structures are interpreted as seismites. The existence of seismites in the Kolankaya Formation is evidence for continuing tectonic activity in the study area during the Neogene and is consistent with the occurrence of the paleoearthquakes of magnitude >5. PMID:25152909

Active Deformation of Malawi Rift's North Basin Hinge Zone Modulated by Reactivation of Preexisting Precambrian Shear Zone Fabric

Science.gov (United States)

Kolawole, F.; Atekwana, E. A.; Laó-Dávila, D. A.; Abdelsalam, M. G.; Chindandali, P. R.; Salima, J.; Kalindekafe, L.

2018-03-01

We integrated temporal aeromagnetic data and recent earthquake data to address the long-standing question on the role of preexisting Precambrian structures in modulating strain accommodation and subsequent ruptures leading to seismic events within the East African Rift System. We used aeromagnetic data to elucidate the relationship between the locations of the 2009 Mw 6.0 Karonga, Malawi, earthquake surface ruptures and buried basement faults along the hinge zone of the half-graben comprising the North Basin of the Malawi Rift. Through the application of derivative filters and depth-to-magnetic-source modeling, we identified and constrained the trend of the Precambrian metamorphic fabrics and correlated them to the three-dimensional structure of buried basement faults. Our results reveal an unprecedented detail of the basement fabric dominated by high-frequency WNW to NW trending magnetic lineaments associated with the Precambrian Mughese Shear Zone fabric. The high-frequency magnetic lineaments are superimposed by lower frequency NNW trending magnetic lineaments associated with possible Cenozoic faults. Surface ruptures associated with the 2009 Mw 6.0 Karonga earthquake swarm aligned with one of the NNW-trending magnetic lineaments defining a normal fault that is characterized by right-stepping segments along its northern half and coalesced segments on its southern half. Fault geometries, regional kinematics, and spatial distribution of seismicity suggest that seismogenic faults reactivated the basement fabric found along the half-graben hinge zone. We suggest that focusing of strain accommodation and seismicity along the half-graben hinge zone is facilitated and modulated by the presence of the basement fabric.

Caracterización de la aloinmunización eritrocitaria en el Hospital Universitario del Valle entre 2011 y 2013 / Characterization of Red Blood Cells Alloimmunization at Hospital Universitario del Valle between 2011 and 2013 / Caracterização de aloimunização eritrocitária no Hospital Universitário do Valle no período de 2011 a 2013

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José Arnulfo Pérez-Carrillo, Esp. MD.

2014-11-01

Full Text Available Introducción: Las necesidades nacionales de sangre están parcialmente cubiertas. El uso de la sangre implica la detección e identificación de anticuerpos inesperados en los receptores de componentes eritrocitarios. Objetivo: Caracterizar demográfica y clínicamente los casos de aloinmunización eritrocitaria en el servicio transfusional del Hospital Universitario del Valle (HUV, Cali, Valle del Cauca, Colombia entre 2011 y 2013. Metodología: Se diseñó un estudio de corte transversal con los casos de aloinmunización eritrocitaria transfundidos por el servicio transfusional del HUV entre el 1 de agosto del 2011 hasta el 31 de julio del 2013. Los casos se incluyeron a través de un muestreo con asignación al azar sistemático. Para ingreso de datos y análisis se empleó el programa Epi-Info para Windows®. El estudio contó con aprobación del Comité de Ética. Resultados: Se incluyeron 80 casos de los cuales el 53.8% eran de género femenino y el 46.2% masculino. Además, el 65% correspondía a raza mestiza hispana y el 35% a afrodescendientes. El 22.5% tenía antecedentes de enfermedades hematopoyéticas y el 45% estaban hospitalizados por diagnósticos incluidos en esta categoría del CIE-10. El 79% de las mujeres tenían historia obstétrica. El 18.75% fueron transfundidos previamente. El 36% de los casos contaba con un fenotipo CceeK. El 31.25% tenían aloanticuerpo Anti-E, seguido por Anti-K con el 21.25%. Conclusiones: El principal aloanticuerpo identificado fue Anti-E seguido de Anti-K. Asimismo existe un grupo importante de pacientes en los cuales no se pudo identificar el aloanticuerpo asociado, debido principalmente a mezcla de anticuerpos. Además, la mayoría de los casos corresponde a adultos jóvenes y adultos. En relación con las características clínicas de la muestra se observó una representación discreta de las hemoglobinopatías congénitas y la mayoría no fueron politransfundidos previamente. [Pérez JA, Cort

SAR Interferometry and Precise Leveling for the Determination of Vertical Displacements in the Upper Rhine Graben Area, Southwest Germany

Science.gov (United States)

Fuhrmann, T.; Schenk, A.; Westerhaus, M.; Zippelt, K.; Heck, B.

2013-12-01

The PS-InSAR (Persistent Scatterer SAR Interferometry) method and precise levelings provide a unique database to detect recent displacements of the Earth's surface. Data of both measurement techniques are analyzed at Geodetic Institute, Karlsruhe Institute of Technology, in order to gain detailed insight into the velocity field of the Upper Rhine Graben (URG). As central and most prominent segment of the European Cenozoic rift system, the seismically and tectonically active Rhine Graben is of steady geo-scientific interest. In the last decades, the URG is characterized by small tectonic movements (Switzerland over the last 100 years building a network of leveling lines. A kinematic network adjustment is applied on the leveling data, providing an accurate solution for vertical displacement rates with accuracies of 0.2 to 0.4 mm/a. The biggest disadvantage of the leveling database is the sparse spatial distribution of the measurement points. Therefore, PS-InSAR is used to significantly increase the number of points within the leveling loops. To obtain a high accuracy for line of sight displacement rates, ERS-1/2 and Envisat data from ascending and descending orbits covering a period from 1992 to 2000 and 2002 to 2010, resp., are processed using StaMPS (Stanford Method for Persistent Scatterers). As the tectonic displacements cover a large area, the separation of atmospheric effects and orbit errors plays an important role in the PS-InSAR processing chain. Besides the tectonic signal, man-induced surface displacements caused by oil extraction are investigated. A comparison between the estimates from leveling and InSAR provides detailed insight into the temporal and spatial characteristics of the surface displacement as well as into the possibilities and limits of the measurement techniques.

Low enthalpy Na-chloride waters from the Lunigiana and Garfagnana grabens, Northern Apennines, Italy: Tracing fluid connections and basement interactions via chemical and isotopic compositions

Science.gov (United States)

Boschetti, Tiziano; Toscani, Lorenzo; Barbieri, Maurizio; Mucchino, Claudio; Marino, Tiziana

2017-12-01

The Na-Cl waters from NW Tuscany (central Italy) record similar water isotopic and major chemical compositions, which demonstrate their meteoric origin and interactions with Upper Triassic evaporites and the metamorphic units of the Paleozoic basement. Slight differences are found in the deep temperature-pressure conditions of the Lunigiana graben (39-42 °C/143-145 bar) and the Garfagnana graben (73-78 °C/250-256 bar). In particular, the thermal fluids outpouring from Garfagnana are probably related to a common deep reservoir or interconnected fluids. Their differences are mainly evidenced by strontium isotopic ratio data (87Sr/86Sr), which combined with previously published sulfur isotope ratios (34S/32S) demonstrate the involvement of vein barites in water-rock interactions. Most likely, these minerals formed during Upper Oligocene-Miocene tectogenesis due to the mixing of fluids from the Verrucano Group and Upper Triassic units. The results of this hydrogeochemical study of the deep Na-Cl fluids could better clarify the distribution of the Verrucano Group within this area and the related discrepancies in the stratigraphic interpretations of the Palaeozoic-Mesozoic transition. Furthermore, the possible presence of an interconnected reservoir could be used to help interpret data produced by the local geochemical monitoring of seismic activity.

El olvido de los silencios negros en el valle del Risaralda 1880-1973

OpenAIRE

Victoria Mena, Carlos Alfonso

2014-01-01

Los procesos de poblamiento y colonización en la cuenca media del valle geográfico del río Cauca, desde el siglo XVIII hasta finales del siglo XIX, dan cuenta de varios fenómenos de los que se debe ocupar la historiografía para desarrollar hipótesis asociadas a tipologías de frontera, como la cimarrona, que de algunas manera se pueden interpretar como rasgos de la configuración de hegemonías comunales y, por tanto, interpelar los enfoques que le otorgan a la colonización antioqueña un carácte...

Recolección y procesamiento de basura en el Valle de El Guarco.

OpenAIRE

Quesada, Hilda; Mora, Benjamín; Hernández, Enrique; Arnáez, Elizabeth; Valverde, Virginia

2016-01-01

En 1987 se realizó un Diagnóstico Socio-ambiental en el Valle de El Guarco, con el propósito de conocer la magnitud y las características de los problemas ambientales en los cantones Central, Paraíso, Oreamuno y El Guarco de la provincia de Cartago y en el que el problema de la basura fue un aspecto por estudiar. La información se recopiló por medio del análisis de estudios realizados, entrevistas a miembros de los gobiernos locales y grupos de base así como giras de inspección ocular y aplic...

Migration history of air-breathing fishes reveals Neogene atmospheric circulation patterns

Science.gov (United States)

Böhme, M.

2004-05-01

The migration history of an air-breathing fish group (Channidae; snakehead fishes) is used for reconstructing Neogene Eurasian precipitation and atmospheric circulation patterns. The study shows that snakeheads are sensitive indicators of summer precipitation maxima in subtropical and temperate regions, and are present regularly if the wettest month exceeds 150 mm precipitation and 20 °C mean temperature. The analysis of 515 fossil freshwater fish deposits of the past 50 m.y. from Africa and Eurasia shows two continental-scale migration events from the snakeheads' center of origin in the south Himalayan region, events that can be related to changes in the Northern Hemisphere circulation pattern. The first migration, ca. 17.5 Ma, into western and central Eurasia may have been caused by a northward shift of the Intertropical Convergence Zone that brought western Eurasia under the influence of trade winds that produced a zonal and meridional precipitation gradient in Europe. During the second migration, between 8 and 4 Ma, into Africa and East Asia, snakeheads reached their present-day distribution. This migration could have been related to the intensification of the Asian monsoon that brought summer precipitation to their migratory pathways in East Africa Arabia and East Asia.

Discontinuous drainage systems formed by highland precipitation and ground-water outflow in the Navua Valles and southwest Hadriacus Mons regions, Mars

Science.gov (United States)

Hargitai, H. I.; Gulick, V. C.; Glines, N. H.

2017-09-01

The Navua Valles are systems of paleodrainages located north of Dao Vallis, which empty into Hellas Planitia, the largest impact basin on Mars. In this study, we mapped and characterized the Navua Valles Region's individual drainage systems, including drainages along the southwestern flank of Hadriacus Mons, and one valley network from the same source as Navua Valles but flowing in the opposite direction. The major drainage systems share morphological characteristics common to both outflow channels and valley networks. The slopes in this region are dissected by two major Navua drainage systems (here Navua A* and B*) and several shorter, sub-parallel valleys formed on the highest gradient (approximately 20 m/km [1.15°]) slopes, at the lowest part of Hellas Basin's rim. The two major drainage systems originate in the highlands, and empty into the basin. Our mapping suggests that water in Navua Valles reached the basin floor in a complicated descent and included several episodes of surface ponding, surface runoff, infiltration, subsurface flow and subsequent outflow. The most prominent channel system, Navua A, forms a repetitive sequence of deep incision into bedrock, followed by a transition into broad channels in erodible materials, and then into unconfined deposits. This successive erosion-transport-deposition sequence continues to repeat along the valley's entire length forming a discontinuous pattern that is consistent with classical fluvial process models. The channels cut into volcanic plains likely emplaced from the formation of Tyrrhenus and Hadriacus Montes. The dendritic source valleys of Navua A originate from the rim of a highland crater while the rest of this subsystem consists of a single, discontinuous channel which is consistent with a single water source zone that likely supplied water for all channels downslope. These drainages may have formed as discontinuous channels, revealing the potential existence of subsurface drainage pathways located

Neogene amphibians and reptiles (Caudata, Anura, Gekkota, Lacertilia, and Testudines from the south of Western Siberia, Russia, and Northeastern Kazakhstan

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Davit Vasilyan

2017-03-01

Full Text Available Background The present-day amphibian and reptile fauna of Western Siberia are the least diverse of the Palaearctic Realm, as a consequence of the unfavourable climatic conditions that predominate in this region. The origin and emergence of these herpetofaunal groups are poorly understood. Aside from the better-explored European Neogene localities yielding amphibian and reptile fossil remains, the Neogene herpetofauna of Western Asia is understudied. The few available data need critical reviews and new interpretations, taking into account the more recent records of the European herpetofauna. The comparison of this previous data with that of European fossil records would provide data on palaeobiogeographic affiliations of the region as well as on the origin and emergence of the present-day fauna of Western Siberia. An overview of the earliest occurrences of certain amphibian lineages is still needed. In addition, studies that address such knowledge gaps can be useful for molecular biologists in their calibration of molecular clocks. Methods and Results In this study, we considered critically reviewed available data from amphibian and reptile fauna from over 40 Western Siberian, Russian and Northeastern Kazakhstan localities, ranging from the Middle Miocene to Early Pleistocene. Herein, we provided new interpretations that arose from our assessment of the previously published and new data. More than 50 amphibians and reptile taxa were identified belonging to families Hynobiidae, Cryptobranchidae, Salamandridae, Palaeobatrachidae, Bombinatoridae, Pelobatidae, Hylidae, Bufonidae, Ranidae, Gekkonidae, Lacertidae, and Emydidae. Palaeobiogeographic analyses were performed for these groups and palaeoprecipitation values were estimated for 12 localities, using the bioclimatic analysis of herpetofaunal assemblages. Conclusion The Neogene assemblage of Western Siberia was found to be dominated by groups of European affinities, such as Palaeobatrachidae

Tectonosedimentary framework of Upper Cretaceous -Neogene series in the Gulf of Tunis inferred from subsurface data: implications for petroleum exploration

Science.gov (United States)

Dhraief, Wissem; Dhahri, Ferid; Chalwati, Imen; Boukadi, Noureddine

2017-04-01

The objective and the main contribution of this issue are dedicated to using subsurface data to delineate a basin beneath the Gulf of Tunis and its neighbouring areas, and to investigate the potential of this area in terms of hydrocarbon resources. Available well data provided information about the subsurface geology beneath the Gulf of Tunis. 2D seismic data allowed delineation of the basin shape, strata geometries, and some potential promising subsurface structures in terms of hydrocarbon accumulation. Together with lithostratigraphic data obtained from drilled wells, seismic data permitted the construction of isochron and isobath maps of Upper Cretaceous-Neogene strata. Structural and lithostratigraphic interpretations indicate that the area is tectonically complex, and they highlight the tectonic control of strata deposition during the Cretaceous and Neogene. Tectonic activity related to the geodynamic evolution of the northern African margin appears to have been responsible for several thickness and facies variations, and to have played a significant role in the establishment and evolution of petroleum systems in northeastern Tunisia. As for petroleum systems in the basin, the Cretaceous series of the Bahloul, Mouelha and Fahdene formations are acknowledged to be the main source rocks. In addition, potential reservoirs (Fractured Abiod and Bou Dabbous carbonated formations) sealed by shaly and marly formations (Haria and Souar formations respectively) show favourable geometries of trap structures (anticlines, tilted blocks, unconformities, etc.) which make this area adequate for hydrocarbon accumulations.

Cyprininae phylogeny revealed independent origins of the Tibetan Plateau endemic polyploid cyprinids and their diversifications related to the Neogene uplift of the plateau.

Science.gov (United States)

Wang, Xuzhen; Gan, Xiaoni; Li, Junbing; Chen, Yiyu; He, Shunping

2016-11-01

Origin and diversification of the Tibetan polyploid cyprinids (schizothoracins) may help us to explore relationships between diversification of the cyprinids and the Tibetan Plateau uplift. Cyprininae phylogeny was analyzed using mitochondrial and nuclear DNA sequences to trace origins of polyploidy and diversifications of schizothoracins. Ancestral states reconstruction for ploidy levels indicated that the Cyprininae was diploid origin and the schizothoracin clades tetraploid origins. There were two diversification rate shifts along with diversification of the cyprinine fishes in response to the Tibetan uplift. The unusual diversification shifts were located to branches subtending the clades of Tibetan polyploid cyprinids. Our analyses suggested that (i) phylogeny of Cyprininae recovered two independent origins of the Tibetan polyploidy schizothoracins; (ii) diversifications of the schizothoracins were closely related to the Neogene uplift of the Tibetan plateau in the following ways: the relatively ancient Late Oligocene-Middle Miocene adaptive radiation may be associated with the uplift of the southern Tibet and Himalaya; the Middle Miocene-Early Pleistocene lineage-specific diversification broadly coincident with major phase of the Neogene Tibetan uplift; and the most recent Pleistocene diversification shift in Schizothorax closely coincident with the successive Kunlun-Huanghe and Gonghe movements of the Tibetan uplift and the glaciation-induced climate oscillations on the plateau.

Permeability in fractured rocks from deep geothermal boreholes in the Upper Rhine Graben

Science.gov (United States)

Vidal, Jeanne; Whitechurch, Hubert; Genter, Albert; Schmittbuhl, Jean; Baujard, Clément

2015-04-01

Permeability in fractured rocks from deep geothermal boreholes in the Upper Rhine Graben Vidal J.1, Whitechurch H.1, Genter A.2, Schmittbuhl J.1, Baujard C.2 1 EOST, Université de Strasbourg 2 ES-Géothermie, Strasbourg The thermal regime of the Upper Rhine Graben (URG) is characterized by a series of geothermal anomalies on its French part near Soultz-sous-Forêts, Rittershoffen and in the surrounding area of Strasbourg. Sedimentary formations of these areas host oil field widely exploited in the past which exhibit exceptionally high temperature gradients. Thus, geothermal anomalies are superimposed to the oil fields which are interpreted as natural brine advection occurring inside a nearly vertical multi-scale fracture system cross-cutting both deep-seated Triassic sediments and Paleozoic crystalline basement. The sediments-basement interface is therefore very challenging for geothermal industry because most of the geothermal resource is trapped there within natural fractures. Several deep geothermal projects exploit local geothermal energy to use the heat or produce electricity and thus target permeable fractured rocks at this interface. In 1980, a geothermal exploration well was drilled close to Strasbourg down to the Permian sediments at 3220 m depth. Bottom hole temperature was estimated to 148°C but the natural flow rate was too low for an economic profitability (geothermal site by drilling five boreholes, three of which extend to 5 km depth. They identified a temperature of 200° C at 5 km depth in the granitic basement but with a variable flow rate. Hydraulic and chemical stimulation operations were applied in order to increase the initial low permeability by reactivating and dissolving sealed fractures in basement. The productivity was considerably improved and allows geothermal exploitation at 165° C and 20 L/s. Recent studies revealed the occurrences of permeable fractures in the limestones of Muschelkalk and the sandstones of Buntsandstein also. For

BACA Project: geothermal demonstration power plant. Final report

Energy Technology Data Exchange (ETDEWEB)

1982-12-01

The various activities that have been conducted by Union in the Redondo Creek area while attempting to develop the resource for a 50 MW power plant are described. The results of the geologic work, drilling activities and reservoir studies are summarized. In addition, sections discussing the historical costs for Union's involvement with the project, production engineering (for anticipated surface equipment), and environmental work are included. Nineteen geothermal wells have been drilled in the Redondo Creek area of the Valles Caldera: a prominent geologic feature of the Jemez mountains consisting of Pliocene and Pleistocene age volcanics. The Redondo Creek area is within a complex longitudinal graben on the northwest flank of the resurgent structural dome of Redondo Peak and Redondo Border. The major graben faults, with associated fracturing, are geologically plausible candidates for permeable and productive zones in the reservoir. The distribution of such permeable zones is too erratic and the locations too imprecisely known to offer an attractive drilling target. Log analysis indicates there is a preferred mean fracture strike of N31W in the upper portion of Redondo Creek wells. This is approximately perpendicular to the major structure in the area, the northeast-striking Redondo Creek graben. The geothermal fluid found in the Redondo Creek reservoir is relatively benign with low brine concentrations and moderate H/sub 2/S concentrations. Geothermometer calculations indicate that the reservoir temperature generally lies between 500/sup 0/F and 600/sup 0/F, with near wellbore flashing occurring during the majority of the wells' production.

Factores que impiden el crecimiento socio económico de la corporación de producción y comercialización agrícola porvenir Valle del Chota en la comunidad de Chota cantón Ibarra; Diseño de un modelo administrativo financiero-contable para la corporación de producción y comercialización ''Porvenir Valle del Chota'', en el 2014.

OpenAIRE

Espinel Ponce, Edison Wilman

2015-01-01

Determinar la situación administrativa y financiera actual de la ''Corporación de Producción y Comercialización Agrícola Porvenir Valle del Chota'' con la finalidad de conocer y comprender el funcionamiento de la Corporación. Diseñar un modelo administrativo financiero, con políticas y procedimientos acorde a los requerimientos de la Corporación de Producción y Comercialización Agrícola ''Porvenir Valle del Chota'', con la finalidad de apoyar su desarrollo. El presente trabajo busca det...

La infección de cangrejos procedentes del valle de Condebamba (Cajamarca por metacercarias de Paragonimus

Directory of Open Access Journals (Sweden)

Manuel Tantaleán V.

2014-06-01

Full Text Available En los meses de febrero y julio de 1973 se colectaron cangrejos del Valle de Condebamba (Cajamarca correspondientes a Pseudothelphusa chilensis, 69 de ellos (34 machos y 35 hembras fueron examinados, buscando metacercarias de Paragonimus; 22 (64.7% de los machos y 29 (28.85 % de las hembras resultaron infectados con metacercarias, o sea 52 (72.46% de los 69 cangrejos estaban infectados, esta cifra es coincidente con la obtenida por Cuba y cols. (1974.

Estudio clínico epidemiológico de bartonelosis humana en el valle del Monzón, Huamalíes, Huánuco

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Abelardo Tejada

2003-12-01

Full Text Available OBJETIVO: Estudiar los casos de bartonelosis humana en valle del Monzón y determinar las especies de Lutzomyia que podrían jugar papel en la transmisión de la enfermedad en la zona. MATERIAL Y MÉTODOS: Se estudió casos de la enfermedad de Carrión en la selva alta del valle del Monzón, provincia de Huamalíes, Huánuco, donde entre 1997 y 1998 se presentó un brote epidémico. Para el diagnóstico de los casos se realizó frotis y gota gruesa, hemocultivo y serología. Para la captura de flebotominos, se utilizó trampas de luz CDC y trampa Shannon, en ambientes intra y peridomiciliarios. RESULTADOS: A lo largo de 21 localidades, la enfermedad afectó 140 personas, 25 de ellos entre 1 y 4 años de edad, 81 mujeres y 59 hombres; 121 presentaron la fase aguda de la enfermedad, 16 la fase intercalar y 3 la fase eruptiva. La población de la zona se dedica principalmente al cultivo de la coca, café y cacao. CONCLUSIÓN: Se estableció que el valle del Monzón es nueva zona endémica de bartonelosis humana, donde la transmisión ocurre principalmente en ambientes intra y peridomiciliarios, siendo Lutzomyia serrana el vector más probable.

Prácticas ambientales de las empresas turísticas en valle de Bravo

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Hernández Peñaloza1 Nadia

2012-05-01

Full Text Available El presente artículo analiza las prácticas ambientales de los actores sociales que se relacionan con las empresas turísticas del municipio de Valle de Bravo, Estado de México. Cabe mencionar que dichas prácticas se consideraron desde el punto de vista socio- económico, es decir, no sólo como se asumen en cuanto al manejo de los recursos naturales, sino también desde su entorno social y económico. Por ello, a partir de la propuesta metodológica de la teoría de sistemas complejos, se analizan los efectos producidos en los entornos de este destino turístico, lo que permite visualizar deuna manera holística la situación que prevalece para al cuidado del ambiente con la participación de todos los actores sociales de la localidad. Los resultados encontrados muestran una gran debilidaden la implementación de dichas prácticas, ya que éstas, actualmente, son impuestas por el gobierno municipal y no se asumen como una iniciativa de los propios actores que participan en las empresas turísticas. Por esta razón, las condiciones de deterioro ambiental en Valle de Bravo son cada vez mayores. A partir de los resultados generados por este estudio, se formulan recomendaciones de implementación y mejoramiento de las prácticas ambientales que contribuyen a la conservación y al cuidado del ambiente.

Neogene Tiporco Volcanic Complex, San Luis, Argentina: An explosive event in a regional transpressive - local transtensive setting in the pampean flat slab

Science.gov (United States)

Ibañes, Oscar Damián; Sruoga, Patricia; Japas, María Silvia; Urbina, y. Nilda Esther

2017-07-01

The Neogene Tiporco Volcanic Complex (TVC) is located in the Sierras Pampeanas of San Luis, Argentina, at the southeast of the Pampean flat-slab segment. Based on the comprehensive study of lithofacies and structures, the reconstruction of the volcanic architecture has been carried out. The TVC has been modeled in three subsequent stages: 1) initial updoming, 2) ignimbritic eruptive activity and 3) lava dome emplacement. Interplay of magma injection and transtensional tectonic deformation has been invoked to reproduce TVC evolution.

Thick-skinned tectonics in a Late Cretaceous-Neogene intracontinental belt (High Atlas Mountains, Morocco): The flat-ramp fault control on basement shortening and cover folding

Science.gov (United States)

Fekkak, A.; Ouanaimi, H.; Michard, A.; Soulaimani, A.; Ettachfini, E. M.; Berrada, I.; El Arabi, H.; Lagnaoui, A.; Saddiqi, O.

2018-04-01

Most of the structural studies of the intracontinental High Atlas belt of Morocco have dealt with the central part of the belt, whose basement does not crop out. Here we study the Alpine deformation of the North Subatlas Zone, which is the part of the Western High Atlas (WHA) Paleozoic Massif that involves both Paleozoic basement units and remnants of their Mesozoic-Cenozoic cover formations. Our aim is to better constrain the geometry and kinematics of the basement faults during the Alpine shortening. Based on detail mapping, satellite imagery and field observations, we describe an array of sub-equatorial, transverse and oblique faults between the WHA Axial Zone and the Haouz Neogene basin. They define a mosaic of basement blocks pushed upon one another and upon the Haouz basement along the North Atlas Fault (NAF). The Axial Zone makes up the hanging-wall of the Adassil-Medinet Fault (AMF) south of this mosaic. The faults generally presents flat-ramp-flat geometry linked to the activation of multiple décollement levels, either within the basement where its foliation is subhorizontal or within favourable cover formations (Jurassic evaporites, Lower Cretaceous silty red beds, Upper Cretaceous evaporitic marls, Neogene basal argillites). The occurrence of the North Atlas detachment (NAD) allowed folded pop-up units to develop in front of the propagating NAF. Shortening began as early as the Campanian-Maastrichtian along the AMF. The direction of the maximum horizontal stress rotated from NNE-SSW to NNW-SSE from the Maastrichtian-Paleocene to the Neogene. The amount of shortening reaches 20% in the Azegour transect. This compares with the shortening amount published for the central-eastern High Atlas, suggesting that similar structures characterize the Paleozoic basement all along the belt. The WHA thick-skinned tectonics evokes that of the frontal Sevier belt and of the external Western Alps, although with a much minor pre-inversion burial.

Anatomy of extremely thin marine sequences landward of a passive-margin hinge zone: Neogene Calvert Cliffs succession, Maryland, U.S.A.

Energy Technology Data Exchange (ETDEWEB)

Kidwell, S.M. [Univ. of Chicago, IL (United States). Dept. of Geophysical Sciences

1997-03-01

Detailed examination of Neogene strata in cliffs 25--35 m high along the western shore of Chesapeake Bay, Maryland, reveals the complexity of the surviving record of siliciclastic sequences {approximately}150 km inland of the structural hinge zone of the Atlantic passive margin. Previous study of the lower to middle Miocene Calvert (Plum Point Member) and Choptank Formations documented a series of third-order sequences 7--10 m thick in which lowstand deposits are entirely lacking, transgressive tracts comprise a mosaic of condensed bioclastic facies, and regressive (highstand) tracts are present but partially truncated by the next sequence boundary; smaller-scale (fourth-order) cyclic units could not be resolved. Together, these sequences constitute the transgressive and early highstand tracts of a larger (second-order Miocene) composite sequence. The present paper documents stratigraphic relations higher in the Calvert Cliffs succession, including the upper Miocene St. Marys Formation, which represents late highstand marine deposits of the Miocene second-order sequence, and younger Neogene fluvial and tidal-inlet deposits representing incised-valley deposits of the succeeding second-order cycle. The St. Marys Formation consists of a series of tabular units 2--5 m thick, each with an exclusively transgressive array of facies and bounded by stranding surfaces of abrupt shallowing. These units, which are opposite to the flooding-surface-bounded regressive facies arrays of model parasequences, are best characterized as shaved sequences in which only the transgressive tract survives, and are stacked into larger transgressive, highstand, and forced-regression sets.

Tectonosedimentary framework of Upper Cretaceous –Neogene series in the Gulf of Tunis inferred from subsurface data: implications for petroleum exploration

Directory of Open Access Journals (Sweden)

Dhraief Wissem

2017-04-01

Full Text Available The objective and the main contribution of this issue are dedicated to using subsurface data to delineate a basin beneath the Gulf of Tunis and its neighbouring areas, and to investigate the potential of this area in terms of hydrocarbon resources. Available well data provided information about the subsurface geology beneath the Gulf of Tunis. 2D seismic data allowed delineation of the basin shape, strata geometries, and some potential promising subsurface structures in terms of hydrocarbon accumulation. Together with lithostratigraphic data obtained from drilled wells, seismic data permitted the construction of isochron and isobath maps of Upper Cretaceous-Neogene strata. Structural and lithostratigraphic interpretations indicate that the area is tectonically complex, and they highlight the tectonic control of strata deposition during the Cretaceous and Neogene. Tectonic activity related to the geodynamic evolution of the northern African margin appears to have been responsible for several thickness and facies variations, and to have played a significant role in the establishment and evolution of petroleum systems in northeastern Tunisia. As for petroleum systems in the basin, the Cretaceous series of the Bahloul, Mouelha and Fahdene formations are acknowledged to be the main source rocks. In addition, potential reservoirs (Fractured Abiod and Bou Dabbous carbonated formations sealed by shaly and marly formations (Haria and Souar formations respectively show favourable geometries of trap structures (anticlines, tilted blocks, unconformities, etc. which make this area adequate for hydrocarbon accumulations.

Isotopic clues to magmatic source regions for neogene Andean volcanic rocks in the El Teniente area near 38oS latitude

International Nuclear Information System (INIS)

Kay, Suzanne Mahlburg; Kurtz, A.C

2001-01-01

The origin of isotopic variations in Central Andean arc lavas is a long-standing problem that involves identifying mantle and crustal source regions. Advances have come from analyzing temporal and spatial variations in constrained tectonic settings. The purpose here is to highlight the similarities of temporal variations in an east-west transect of Neogene magmatic units near 34 O S latitude with those from a south-north transect along the modern Southern Volcanic Zone (SVZ, e.g. Hildreth and Moorbath 1988, Tormey et al. 1991). The comparison shows the importance of crustal thickening processes associated with compressional shortening and of lithospheric scale adjustments associated with eastward migration of the arc front on magma sources. Sr, Nd and Pb isotopic analyses of 27 Neogene volcanic and plutonic samples from the El Teniente area are presented in Table 1 and plotted along with some analyses from Skewes and Stern (1994) and Stern and Skewes (1995) in Figure 2. The data show a clear progression from older samples with more 'depleted' isotopic signatures (lower 87 Sr/ 86 Sr and Pb isotopic ratios, higher εNd) to younger samples with more 'enriched' signatures (higher 87 Sr/ 86 Sr and Pb isotopic ratios, lower εNd). In detail, four temporal and spatial groups marked by discontinuities in isotopic trends can be defined. Within each group, εNd tends to decrease and 87 Sr/ 86 Sr ratios to increase with SiO2 concentration (au)

Eos Chaos Rocks

Science.gov (United States)

2006-01-01

11 January 2006 This Mars Global Surveyor (MGS) Mars Orbiter Camera (MOC) image shows light-toned, layered rock outcrops in Eos Chaos, located near the east end of the Valles Marineris trough system. The outcrops occur in the form of a distinct, circular butte (upper half of image) and a high slope (lower half of image). The rocks might be sedimentary rocks, similar to those found elsewhere exposed in the Valles Marineris system and the chaotic terrain to the east of the region. Location near: 12.9oS, 49.5oW Image width: 3 km (1.9 mi) Illumination from: lower left Season: Southern Summer

Estudios sobre la enfermedad de Carrión en el valle interandino del Mantaro: II. Incidencia de la infección bartonelosica en la población humana

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Arístides Herrer

1960-01-01

Full Text Available Con la finalidad de determinar la zona endémica de la verruga peruana o enfermedad de Carrión en el valle del Mantaro, durante la segunda quincena de abril. 1959, se realizaron 239 hemocultivos y una encuesta informativa en la población del mencionado valle. Para los cultivos se obtuvo 215 muestras de sangre en la población humana y, las 24 restantes, en algunos animales domésticos. En la encuesta se trató de recoger las informaciones que la gente de la región podría ofrecer acerca de la verruga, al mismo tiempo que todas las personas encuestadas fueron revisadas por los autores en busca del brote verrucoso. Los siguientes son los principales resultados obtenidos: 1. En los cultivos con sangre humana se obtuvo 5 positivos, 172 negativos y 38 contaminados y. en la de los animales domésticos, 13 negativos y 11 contaminados. Todos los hemocultivos positivos correspondieron a personas que habitan en localidades que se hallan entre 2.800 y 3,000 metros de altitud. 2. Dos de las cinco personas que ofrecieran hemocultivo positivo, al momento de extraérseles la sangre se encontraban en estado febril y con abundantes bartonelas en los eritrocitos circulantes; ambas murieron pocos días después. Las tres restantes no presentaban síntomas atribuibles a la enfermedad de Carrión, y dos de ellas fueron observadas durante los 15 meses subsiguientes sin que presentasen brote verrucoso. 3. En la encuesta se verificó que, con rarísimas excepciones, la gente del valle del Mantaro no conocía la verruga. Del mismo modo, tan sólo en dos ocasiones los autores observaron nódulos subcutáneos semejantes a verrucomas. 4. Se hace resaltar el que la enfermedad de Carrión sea endémica a considerable altitud en el valle del Mantaro, así como la rareza del brote cutáneo y se cuestiona la extrema gravedad que se atribuye a la verruga en el referido valle del Mantaro.

La inserción al Asia-Pacífico, oportunidades y desafíos para el Valle del Cauca y la región pacífica colombiana

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Ricardo Coutin

2014-12-01

Full Text Available Resumen: El objetivo general del texto es brindar una aproximación a los retos y las oportunidades que representa, para el Valle del Cauca y la Región Pacífica colombiana, la inserción al Asia-Pacífico. Para lo cual se plantean tres objetivos específicos: primero, analizar someramente el contexto económico comercial del Asia-Pacífico y América Latina, con especial énfasis en Colombia y los demás países de la Alianza del Pacífico (AP; segundo, estudiar las oportunidades y los retos para el Valle del Cauca y la Región Pacífica colombiana que plantea la puesta en escena del bloque comercial denominado Alianza del Pacífico; y tercero, indagar sobre los retos de competitividad y productividad que enfrenta el Valle del Cauca y que afectan el ambiente de negocios. El documento concluye que Colombia se encuentra rezagada en su inserción con la cuenca del Asia-Pacífico; también se plantea la necesidad de abordar el tema de estudio desde un enfoque subnacional.

Seismic chimneys in the Southern Viking Graben - Implications for palaeo fluid migration and overpressure evolution

Science.gov (United States)

Karstens, Jens; Berndt, Christian

2015-02-01

Detailed understanding of natural fluid migration systems is essential to minimize risks during hydrocarbon exploration and to evaluate the long-term efficiency of the subsurface storage of waste water and gas from hydrocarbon production as well as CO2. The Southern Viking Graben (SVG) hosts numerous focused fluid flow structures in the shallow (expressions of vertical fluid conduits are variously known as seismic chimneys or pipes. Seismic pipes are known to form large clusters. Seismic chimneys have so far been described as solitary structures. Here, we show that the study area in the SVG hosts more than 46 large-scale vertical chimney structures, which can be divided in three categories implying different formation processes. Our analysis reveals that seal-weakening, formation-wide overpressure and the presence of free gas are required to initiate the formation of vertical fluid conduits in the SVG. The presence of numerous vertical fluid conduits implies inter-stratigraphic hydraulic connectivity, which significantly affects the migration of fluids in the subsurface. Chimney structures are important for understanding the transfer of pore pressure anomalies to the shallow parts of the basin.

Prevalence of school desertion during teenage pregnancy from public schools in Valle del Cauca, 2006

OpenAIRE

Iván Osorio; Mauricio Hernández

2011-01-01

Antecedentes: Partiendo de la institución educativa, se investigó la relación entre embarazo adolescente y deserción escolar y como influía el grado escolar y la edad de la embarazada en su riesgo de deserción. Materiales y métodos: Se aplicó una encuesta voluntaria en 180 instituciones educativas oficiales del departamento del Valle del Cauca, correspondiente a 112,470 estudiantes mujeres, encontrando 605 embarazadas. De estas, a 564 se les realizó una entrevista por un profesional en psicol...

Definición del mercado de trigo cristalino en el valle del Yaqui, México

OpenAIRE

Garza Lagler, María Cristina; Taddei Bringas, Cristina

2016-01-01

Resumen: El valle del Yaqui es una región productora de trigo en el noroeste de México, cuyas agroempresas tienen una participación creciente en el mercado internacional. El objetivo de este trabajo es una aproximación a la definición del mercado del trigo cristalino que se produce en su territorio, para lo cual se realizó un análisis descriptivo apoyado en entrevistas a actores estratégicos del sistema de producción. Los resultados indican que este grano tiene tres mercados: la industria de ...

La inserción al Asia-Pacífico, oportunidades y desafíos para el Valle del Cauca y la región pacífica colombiana

OpenAIRE

Countin, Ricardo

2014-01-01

El objetivo general del texto es brindar una aproximación a los retos y las oportunidades que representa, para el Valle del Cauca y la Región Pacífica colombiana, la inserción al Asia-Pacífico. Para lo cual se plantean tres objetivos específicos: primero, analizar someramente el contexto económico comercial del Asia-Pacífico y América Latina, con especial énfasis en Colombia y los demás países de la Alianza del Pacífico (AP); segundo, estudiar las oportunidades y los retos para el Valle del C...

Secular Trends of Amyotrophic Lateral Sclerosis: The Piemonte and Valle d'Aosta Register.

Science.gov (United States)

Chiò, Adriano; Mora, Gabriele; Moglia, Cristina; Manera, Umberto; Canosa, Antonio; Cammarosano, Stefania; Ilardi, Antonio; Bertuzzo, Davide; Bersano, Enrica; Cugnasco, Paolo; Grassano, Maurizio; Pisano, Fabrizio; Mazzini, Letizia; Calvo, Andrea

2017-09-01

This study reports the long-term epidemiologic trends of amyotrophic lateral sclerosis (ALS) based on a prospective register. To examine the 20-year epidemiologic trends of ALS in the Piemonte and Valle d'Aosta regions of Italy. The Piemonte and Valle d'Aosta Register for ALS (PARALS) is an epidemiologic prospective register that covers 2 Italian regions (population of 4 476 931 inhabitants according to the 2011 census) from January 1, 1995, through December 31, 2014. Case ascertainment is based on multiple sources (neurologic departments, hospital discharge archives, and mortality records). Incidence rates are age and sex standardized for the Italian population of the 2011 census. Age-period-cohort (APC) analysis was performed using a Poisson regression model. The primary study outcomes were long-term incidence and prevalence rates of ALS using a prospective design and their determinants. During the study period, a total of 2702 patients (mean [SD] age at onset, 65.7 [11.1] years; 1246 [46.1%] female and 1456 [53.9%] male) received a diagnosis of ALS between 1995 and 2014, corresponding to a crude annual incidence rate of 3.03 per 100 000 population (95% CI, 2.85-3.23) and an adjusted incidence rate of 2.78 per 100 000 population (95% CI, 2.57-2.96). The age-adjusted incidence rate increased in the 2 decades of the study (1995-2004: 2.66; 95% CI, 2.50-2.83; 2005-2014: 2.89; 95% CI, 2.71-3.07; P = .04), mostly in women. The adjusted rate ratio of men to women decreased from 1.27:1 (1995-2004) to 1.17:1 (2005-2014). The analysis of deviance for the APC regression models indicated that the drift variable is relevant in explaining the variation of ALS incidence rates over time in the overall population (change in deviance, 4.6553; P = .03) and in women (change in deviance, 3.8821; P = .05) but not in men (change in deviance, 0.77215; P = .38). A total of 479 patients with ALS were alive and had not undergone tracheostomy at the prevalence day

Public views and attitudes concerning fire and fuels reduction strategies in the Valles Caldera National Preserve (VCNP) New Mexico

Science.gov (United States)

Kurt Anschuetz; Carol Raish

2010-01-01

The Valles Caldera National Preserve (VCNP), located in the heart of the Jemez Mountains in northcentral New Mexico, is a special place for many residents of the region. The large volcanic caldera, formerly the privately owned Baca Ranch, is an 89,000-acre property known for its scenic meadows and abundant wildlife, including herds of elk. The U.S. purchased the...

Església i poder comtal al territori d’Urgell. Guifré el Pilós i la reorganització de la Vall de Lord

Directory of Open Access Journals (Sweden)

Riu, Manuel

1999-12-01

Full Text Available This article shows how was "La Vall de Lord" organized in four castles, their respective territories and ten rural parish churches and also their evolution during the ninth and tenth centuries. It explains the exemption land taxes in the southern part of the Urgell's county and bishopric, and the relievant role of Guifred "el Pilos" count and Seu bishops in that establishment. Two bénédictine monasteries, Sant Llorenç de Morunys and Sant Pere de Graudescales, had an important development in the "Vail de Lord". At the first time, both were regular priests'canonicals.[fr] Dans cet article, on présente l'organisation de la Vallée de Lord en quatre chatellenies et dix paroisses, et leur évolution pendant les IXème et Xème siècles, en indiquant le statut de zone franche dans la limite méridionale du comté et évêché d'Urgell, et le rôle notoire du comte Guifred "el Pilos" et des prélats de La Seu. Dans la vallée prirent leur essor également deux monastères bénédictins, celui de Sant Llorenç de Morunys et celui de Sant Pere de Graudescales, qui furent initialement des chapitres de clercs réguliers.

Evaluación de los programas de control prenatal para adolescentes en el valle de Aburrá, 2003 Evaluation of prenatal control programs offered to teenagers in Valle de Aburrá, Colombia, 2003

Directory of Open Access Journals (Sweden)

Carlos Adolfo Salazar

2004-02-01

Full Text Available Objetivo: la investigación que se presenta a continuación tuvo como objetivo identificar y evaluar los programas de control prenatal para adolescentes ofrecidos en el valle de Aburrá, Antioquia, Colombia, durante el año 2003. Materiales y métodos: se revisaron varias fuentes primarias y se elaboró un listado de todas las instituciones de salud del valle de Aburrá. Se hicieron entrevistas telefónicas con los respectivos directores para establecer cuáles instituciones tenían un programa de control prenatal exclusivo para adolescentes y a estas instituciones se les aplicó un formato de evaluación para determinar si cumplían con los estándares internacionales descritos en la literatura como esenciales en un programa de control prenatal para adolescentes. Resultados: sólo una de las 101 instituciones de salud que ofrecían control prenatal tenía un programa exclusivo para adolescentes. Sin embargo, a la luz de la evaluación, dicho programa no cumplía con los estándares de un programa de control prenatal para adolescentes. Conclusión: a pesar de que en Colombia el embarazo en adolescentes es un problema de salud pública, los programas de control prenatal para adolescentes no se han implementado en el valle de Aburrá. Establecerlos constituye una de las estrategias para resolver esta problemática. Objective : this investigation had the aim of identifying and evaluating the prenatal control programs offered to teenagers in the Aburrá Valley region of Colombia in 2003. Methodology: through various sources a list was compiled which included all the health institutions in the Aburrá Valley region. The institutions which offered exclusive teenage prenatal control were identified by telephone and a questionnaire was applied to them with the purpose of knowing if they met the international standards described in relevant sources as being essential in a teenage prenatal control program. Results: in only one of the 101 health

Project Half Double

DEFF Research Database (Denmark)

Svejvig, Per; Ehlers, Michael; Adland, Karoline Thorp

activities carried out within the framework of the projects. The formal part of Project Half Double was initiated in June 2015. We started out by developing, refining and testing the Half Double methodology on seven pilot projects in the first phase of the project, which will end June 2016. The current......Project Half Double has a clear mission to succeed in finding a project methodology that can increase the success rate of our projects while increasing the speed at which we generate new ideas and develop new products and services. Chaos and complexity should be seen as a basic condition...... and as an opportunity rather than a threat and a risk. We are convinced that by doing so, we can strengthen Denmark’s competitiveness and play an important role in the battle for jobs and future welfare. The overall goal is to deliver “projects in half the time with double the impact”, where projects in half the time...

The Mineral Character and Geomechanical Properties of the Transitional Rocks from the Mesozoic-Neogene Contact Zone in the Bełchatów Lignite Deposit

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Agnieszka Pękala

2014-01-01

Originality/value: Against the background of a number of published papers on the rocks accompanying lignite seams there is a lack of the "Bełchatów" mineralogical-petrographic studies of the transitional sediments in the Mesozoic-Neogene contact zone in the "Bełchatów" lignite deposit taking into account the aspect of raw materials. This paper has been produced to fill the void in this area.

Magnetic Half-Monopole Solutions

International Nuclear Information System (INIS)

Teh, Rosy; Lim, Kok-Geng; Koh, Pin-Wai

2009-01-01

We present exact SU(2) Yang-Mills-Higgs monopole solutions of one half topological charge. These non-Abelian solutions possess gauge potentials which are singular along either the positive or the negative z-axis and common magnetic fields that are singular only at the origin where the half-monopole is located. These half-monopoles are actually a half Wu-Yang monopole and they can possess a finite point electric charge and become half-dyons. They do not necessarily satisfy the first order Bogomol'nyi equations and they possess infinite energy density at r = 0.

Perspectiva bioenergética de los residuos sólidos urbanos en el Valle de Lerma

OpenAIRE

Manrique, Silvina Magdalena; Franco, Ada Judith; Núñez, Virgilio; Seghezzo, Lucas

2017-01-01

Los residuos sólidos urbanos (RSU), que tradicionalmente se han depositado a cielo abierto en el Valle de Lerma (Salta), podrían comenzar a ser dispuestos en un relleno sanitario regional en función de un proyecto provincial existente. El mencionado proyecto no incluye el aprovechamiento de la energía contenida en los RSU. En este trabajo se consideraron como recursos bioenergéticos potenciales. Dos clases de estimaciones fueron realizadas a partir de diferentes metodologías: a) poder caloríf...

paleopatológico del antiguo Valle de Toluca, México

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Héctor Favila Cisneros

2008-01-01

ciénega del Chignahuapan de la Cuenca del Alto Lerma, ahora cabecera municipal de Santa Cruz Atizapan, Estado de México, se desarrolló una sociedad isleña con un modo de vida lacustre, en la cual su equilibrio estaba determinado por la interrelación con el aprovechamiento de los recursos de la laguna y las difíciles condiciones del cenagal. El análisis morfoscópico realizado en las osamentas provenientes de los entierros del sitio arqueológico "La Campana Tepozoco" arrojó una serie de evidencias patológicas, que permiten conocer las condiciones generales de la salud de los habitantes del sitio. La presente investigación nos acerca al conocimiento de las diversas condiciones de existencia, donde el modo de vida impactó en la salud y nutrición de los miembros de esta población de la zona pantanosa de la antigua ciénega del Valle de Toluca.

Local magnitude scale for Valle Medio del Magdalena region, Colombia

Science.gov (United States)

Londoño, John Makario; Romero, Jaime A.

2017-12-01

A local Magnitude (ML) scale for Valle Medio del Magdalena (VMM) region was defined by using 514 high quality earthquakes located at VMM area and inversion of 2797 amplitude values of horizontal components of 17 stations seismic broad band stations, simulated in a Wood-Anderson seismograph. The derived local magnitude scale for VMM region was: ML =log(A) + 1.3744 ∗ log(r) + 0.0014776 ∗ r - 2.397 + S Where A is the zero-to-peak amplitude in nm in horizontal components, r is the hypocentral distance in km, and S is the station correction. Higher values of ML were obtained for VMM region compared with those obtained with the current formula used for ML determination, and with California formula. With this new scale ML values are adjusted to local conditions beneath VMM region leading to more realistic ML values. Moreover, with this new ML scale the seismicity caused by tectonic or fracking activity at VMM region can be monitored more accurately.

Chemical weathering of palaeosols from the Lower Palaeolithic site of Valle Giumentina, central Italy

Science.gov (United States)

Degeai, Jean-Philippe; Villa, Valentina; Chaussé, Christine; Pereira, Alison; Nomade, Sébastien; Aureli, Daniele; Pagli, Marina; Nicoud, Elisa

2018-03-01

The major archaeological site of Valle Giumentina (Abruzzo) contains a well-dated Lower Palaeolithic pedosedimentary sequence that provides an excellent opportunity to study the relationships among soil weathering, volcanism and climate change at the glacial/interglacial and submillennial timescales in central Italy and the Mediterranean area during the Middle Pleistocene, as well as the human-environment interactions of some of the earliest settlements in central southern Europe. High-resolution analyses of geochemistry and magnetic susceptibility revealed the presence of eleven palaeosols, ten of which (S2-S11) were formed between 560 and 450 ka based on 40Ar/39Ar dating of sanidine in tephras, i.e. spanning marine isotope stages (MIS) 14-12. The evolution of the major and trace element composition suggests that the palaeosols were mainly formed by in situ weathering of the parent material. The major phases of soil weathering occurred during the MIS 13 interglacial period (S8 and S6) as well as during episodes of rapid environmental change associated with millennial climatic oscillations during the MIS 14 and 12 glaciations (S11 and S2, respectively). Although global forcing such as orbital variations, solar radiation, and greenhouse gas concentrations may have influenced the pedogenic processes, the volcanism in central Italy, climate change in the central Mediterranean, and tectono-sedimentary evolution of the Valle Giumentina basin also impacted and triggered the formation of most palaeosols, which provided subsistence resources for the Lower Palaeolithic human communities. This study highlights the importance of having high-resolution palaeoenvironmental records with accurate chronology as close as possible to archaeological sites to study human-environment interactions.

Dalla politica alla gestione del bene comune. L’esempio del teatro Valle a Roma

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Alice Furlan

2015-11-01

Full Text Available The concept of common good could be declined in three major points: 1 the theft of the good itself from the profit mindset; 2 the creation of a link between the community and the good; 3 the creation of a new management form, neither public nor private, which knows the capacity of the good itself. From the analysis of the schedule published by MiBAC, it is clear that there is a lack of founds addressed to the artistic research. The situation that occurs nowadays is imposing the necessity of identifying another kind of development model. I took, as a research topic, Teatro Valle, which is one of the most important case in the Italian national context. The management of the entire structure undergoes through the principles of non-rivalry, non-exclusion and self-governance. The strongest points of this model are: the idea of an alternative management and the creation of synergies between several cultural movements.The theatre itself has been seeing as a multi-functional location: there are lots of performances flanked by debates, conferences, talks, and other initiatives. Another important aspect is the great visibility that the experience has been receiving through the years. However it is necessary to underline that the building, which is a private property, lives in a condition of lawlessness because it has been occupied. Moreover Teatro Valle has been accused of unfair competition by other cultural spaces. Since the culture is the common thread that helps us to uphold our identity, the common goods help us to recognize ourselves and state our fundamental rights.

Los «verracos» del valle del Amblés (Ávila: del análisis espacial a la interpretación socio-económica

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Álvarez Sanchís, Jesús R.

1990-12-01

Full Text Available Until recently, the zoomorphic sculpture of the West Meseta has been studied typologically, and therefore out of the cultural context in which it was produced. This paper is concerned with the zoomorphic sculpture in the Valle del Amblés (Ávila. We consider the sculptures as an index of economic value —cattle— and by studying their spatial distribution, we propose that they were used as landmarks or as delimiting critical resources —pasture— the explotation of which could have been organized by the elites of the Second Iron Age communities living in the valley.

La escultura zoomorfa de la Meseta Occidental ha sido tradicionalmente estudiada en su dimensión tipológica y, en consecuencia, divorciada de la dinámica cultural que la produjo. Este trabajo, que tiene su marco geográfico en el Valle del Amblés (Ávila, considera las manifestaciones zoomorfas como el exponente de un valor productivo —la ganadería—; y, mediante el análisis de su distribución espacial, propone la hipótesis de considerarlas hitos o delimitadores de recursos críticos —pastos—, cuya explotación sería organizada por las élites de las comunidades de la II Edad del Hierro que poblaban el valle.

Half-width at half-maximum, full-width at half-maximum analysis

Indian Academy of Sciences (India)

addition to the well-defined parameter full-width at half-maximum (FWHM). The distribution of ... optical side-lobes in the diffraction pattern resulting in steep central maxima [6], reduc- tion of effects of ... and broad central peak. The idea of.

Late Neogene marine incursions and the ancestral Gulf of California

Science.gov (United States)

McDougall, K.

2008-01-01

The late Neogene section in the Salton Trough, California, and along the lower Colorado River in Arizona is composed of marine units bracketed by nonmarine units. Microfossils from the marine deposits indicate that a marine incursion inundated the Salton Trough during the late Miocene. Water depths increased rapidly in the Miocene and eventually flooded the region now occupied by the Colorado River as far north as Parker, Arizona. Marine conditions were restricted in the Pliocene as the Colorado River filled the Salton Trough with sediments and the Gulf of California assumed its present configuration. Microfossils from the early part of this incursion include a diverse assemblage of benthic foraminifers (Amphistegina gibbosa, Uvigerina peregrina, Cassidulina delicata, and Bolivina interjuncta), planktic foraminifers (Globigerinoides obliquus, G. extremus, and Globigerina nepenthes), and calcareous nannoplankton (Discoaster brouweri, Discoaster aff. Discoaster surculus, Sphenolithus abies, and S. neoabies), whereas microfossils in the final phase contain a less diverse assemblage of benthic foraminifers that are diagnostic of marginal shallow-marine conditions (Ammonia, Elphidium, Bolivina, Cibicides, and Quinqueloculina). Evidence of an earlier middle Miocene marine incursion comes from reworked microfossils found near Split Mountain Gorge in the Fish Creek Gypsum (Sphenolithus moriformis) and near San Gorgonio Pass (Cyclicargolithus floridanus and Sphenolithus heteromorphus and planktic foraminifers). The middle Miocene incursion may also be represented by the older marine sedimentary rocks encountered in the subsurface near Yuma, Arizona, where rare middle Miocene planktic foraminifers are found. ?? 2008 The Geological Society of America.

Comunidades liquénicas como bioindicadores de calidad del aire del Valle de Aburrá

Directory of Open Access Journals (Sweden)

Jaramillo Ciro1 Margarita María

2011-11-01

Full Text Available Los líquenes han sido propuestos como bioindicadores de la calidad del aire por su alta sensibilidad a los cambios que afectan su abundancia, biomasa y vitalidad. Para evaluar las afectaciones que los líquenes manifiestan como consecuencia de la contaminación atmosférica, se seleccionaron dos áreas de muestreo en los alrededores de dos estaciones de la red de monitoreo de calidad del aire RedAire: el edificio Miguel de Aguinaga con alta contaminación y la Universidad de Medellín con baja contaminación. El monitoreo se realizó sobre las cortezas de 4 especies arbóreas como forofitos: Terminalia catappa Linneaus, Eritrina fusca Loureiro, Mangifera indica Linneaus y Fraxinus chinensis Roxb. Para los análisis se consideraron las variables cobertura liquénica por especie, vitalidad y fructificación del talo. Finalmente los datos de cobertura fueron utilizados para determinar el índice de pureza atmosférica (IPA y el factor Q. Los resultados evidenciaron que de las 8 especies de líquenes encontradas, Canoparmelia sp. y Parmotrema austrosinensis (Zahlbr Hale. son las más sensibles y apropiadas para estudios de calidad del aire en el Valle de Aburrá. Los análisis estadísticos realizados a los valores de abundancia relativa por forofito mostraron que Fraxinus chinensis Roxb es la especie vegetal portante más apropiada para estudios de líquenes bioindicadores en el Valle de Aburrá.

CULTO A LA VIRGEN DEL VALLE COMO CREENCIA AUTÓCTONA EN LAS ISLAS ORIENTALES VENEZOLANAS

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Natalia Bondarenko

2016-01-01

Full Text Available Se analiza el origen del culto a la Virgen del Valle en el estado insular Nueva Esparta (Venezuela y su relación con las creencias autóctonas de los indígenas guaiqueríes, por un lado, y la creencia católica clásica en la Virgen María, por el otro. Luego de describir la religiosidad de los guaiqueríes en la época prehispánica y presentar las características de la creencia en la Virgen María en la España medieval, se argumenta que el culto a la Virgen se inició en Venezuela en el período colonial, cuando algunos guaiqueríes la aceptaron debido a su semejanza con los cemíes y el carácter matriarcal de su sociedad, para luego, en el período republicano, adherirse masiva y definitivamente a la Virgen, incorporándola a su panteón de divinidades a partir de un suceso histórico insólito. Ellos rendían culto a la Virgen a su modo ancestral, por lo cual esta creencia no puede ser considerada como sincrética. Se concluye que en las islas neoespartanas, aunque con el nombre de una Virgen católica, el culto a la Virgen del Valle representa una creencia autóctona guaiquerí que persiste a través del tiempo, desplegando aspectos católicos solo en los rituales formales de la iglesia.

Petrology, geochemistry and radiometric ages of high silica Adakitic Domes of Neogene continental arc, south of Quchan

International Nuclear Information System (INIS)

Ghasemi, H.; Sadeghian, M.; Khanalizadeh, A.; Tanha, A.

2010-01-01

Neogene high silica adakitic domes of south Quchan, cropped out in the northern part of the Quchan-Esfarayen Cenozoic magmatic arc (north of Sabzevar ophiolitic and metamorphic belt). In this volcanic belt, magmatic activities has been started since Eocene (about 40 Ma ago) and continued to Plio-Pleistocene (about 2 Ma ago). The ages of volcanic rocks range from Eocene to Plio-Pleistocene from south (in adjacent to the Sabzevar ophiolitic belt) to north (in south of Quchan) respectively. Northern part of this high silica adakitic arc is composed of pyroclastic units and several domes contain trachyandesites, trachytes, dacites and rhyodacites (2-12 Ma ago) which are usually overlain an olivine basaltic- basaltic basement of Eocene to Lower Miocene (19-20 Ma ago). Existence of Eocene volcanic enclaves and gneissic, siltstone, marl and pellitic enclaves, appearance and disappearance of some mineral phases, corrosions and chemical dis equilibriums of some phenocrysts and sieve textures are some evidences of magmatic contamination. 87 Sr/ 86 Sr ratio ranges from 0.7041 to 0.7057 confirms this contamination. A clear positive anomaly in LREE and LILE and a negative anomaly in HREE found in the rocks of Neogene domes. Negative anomalies in HFSE (e.g. P, Nb, Ti) which is the indicator of arc settings, also found in these rocks. Calc-alkaline nature, continental arc subduction setting, presence of an eclogitic or garnet-amphibolitic source rock (resulted from metamorphism of Sabzevar subducted oceanic crust as a source of magma generation), high silica adakitic nature of magmatism and the role of fractional crystallization, assimilation and magmatic contamination in the genesis and evolution of magma in these domes, indicated by the geochemical evidences. These adakitic magmas were the latest melts resulted from partial melting of young and hot Sabzevar Neotethyan subducted oceanic crust and its overlaying mantle wedge, which have been emplaced and manifested in the form of

Red Piloto de Información Hidrometeorológica para el Valle de Aburrá.

OpenAIRE

Jiménez Mejía, José Fernando; Ramírez, Carlos Julio; Ochoa Jaramillo, Andrés; Poveda Jaramillo, Germán; Zapata Jaramillo, Carlos Mario; Marín Morales, María Isabel

2008-01-01

El Aula Taller de Ciencia y Tecnología de la Escuela del Maestro (Municipio de Medellín) y el Aula Taller Leonardo Da Vinci (Universidad Nacional de Colombia, Sede Medellín) vienen trabajando desde hace varios años en una propuesta pedagógica novedosa para el estudio de las ciencias naturales. Esta iniciativa dio origen a una red preliminar de estaciones meteorológicas didácticas en más de diez colegios y escuelas en municipios del Valle de Aburrá, las cuales están en funcionamiento. Este pro...

DINÁMICA NUTRICIONAL EN CINCO PARRONES DE DIFERENTE PRODUCTIVIDAD DEL VALLE CENTRAL REGADO DE CHILE

OpenAIRE

Ruiz S., Rafael

2000-01-01

Se efectuó un estudio comparativo de aspectos nutricionales del suelo y de la planta en 5 parronales de uva de mesa cv. Thompson Seedless con un historial muy diferente de productividad y vigor, en el valle central de Chile, durante 4 años. Durante este período se efectuaron análisis nutricionales mensuales, que incluyeron además de N, P y K total, fracciones de N de reserva como arginina y aminoácidos totales y carbohidratos de reserva en la parte aérea (sarmientos y brotes) y en raíces. El ...

La gestión tecnológica: una herramienta para el desarrollo de la Cadena Productiva del Ají en el Valle del Cauca

Directory of Open Access Journals (Sweden)

Omar Rada Barona

2011-01-01

diferentes actores: Secretaría de Agricultura de la Gobernación del Valle del Cauca, Fundación Carvajal, y a la Asociación de Productores y Comercializadores Agrícolas - Agrovac. Como resultado, se observa que la cadena productiva del ají, en el Valle del Cauca, adolece de la aplicación de herramientas tecnológicas que permitan identificar nuevos mercados y analizar la capacidad de la competencia de los productores. El desarrollo de la fase 1: Identificación de la Cadena Productiva del Ají, permite concluir que es necesario implementar la gestión tecnológica en cada uno de los procesos de la cadena, a partir del empoderamiento de los agricultores que participan en la Asociación de Productores y Comercializadores Agrícolas, Agrovac, para que éstos realmente aprovechen las oportunidades de crecimiento y desarrollo.

Upper Neogene stratigraphy and tectonics of Death Valley — a review

Science.gov (United States)

Knott, J. R.; Sarna-Wojcicki, A. M.; Machette, M. N.; Klinger, R. E.

2005-12-01

New tephrochronologic, soil-stratigraphic and radiometric-dating studies over the last 10 years have generated a robust numerical stratigraphy for Upper Neogene sedimentary deposits throughout Death Valley. Critical to this improved stratigraphy are correlated or radiometrically-dated tephra beds and tuffs that range in age from > 3.58 Ma to Mormon Point. This new geochronology also establishes maximum and minimum ages for Quaternary alluvial fans and Lake Manly deposits. Facies associated with the tephra beds show that ˜3.3 Ma the Furnace Creek basin was a northwest-southeast-trending lake flanked by alluvial fans. This paleolake extended from the Furnace Creek to Ubehebe. Based on the new stratigraphy, the Death Valley fault system can be divided into four main fault zones: the dextral, Quaternary-age Northern Death Valley fault zone; the dextral, pre-Quaternary Furnace Creek fault zone; the oblique-normal Black Mountains fault zone; and the dextral Southern Death Valley fault zone. Post - 3.3 Ma geometric, structural, and kinematic changes in the Black Mountains and Towne Pass fault zones led to the break up of Furnace Creek basin and uplift of the Copper Canyon and Nova basins. Internal kinematics of northern Death Valley are interpreted as either rotation of blocks or normal slip along the northeast-southwest-trending Towne Pass and Tin Mountain fault zones within the Eastern California shear zone.

Neogene to recent contraction and basin inversion along the Nubia-Iberia boundary in SW Iberia

Science.gov (United States)

Ramos, Adrià; Fernández, Oscar; Terrinha, Pedro; Muñoz, Josep Anton

2017-02-01

The SW of Iberia is currently undergoing compression related to the convergence between Nubia and Iberia. Multiple compressive structures, and their related seismic activity, have been documented along the diffuse Nubia-Iberia plate boundary, including the Gorringe bank west of the Gulf of Cadiz, and the Betic-Rif orogen to the east. Despite seismic activity indicating a dominant compressive stress along the Algarve margin in the Gulf of Cadiz, the structures at the origin of this seismicity remain elusive. This paper documents the contractional structures that provide linkage across the Gulf of Cadiz and play a major role in defining the present-day seismicity and bathymetry of this area. The structures described in this paper caused the Neogene inversion of the Jurassic oblique passive margin that formed between the central Atlantic and the Ligurian Tethys. This example of a partially inverted margin provides insights into the factors that condition the inversion of passive margins.

The Neogene genus Streptochilus (Brönnimann and Resig, 1971) from the Gulf of California

Science.gov (United States)

Miranda Martínez, A.Y.; Carreño, A.L.; McDougall, Kristin

2017-01-01

Four species of the planktonic foraminiferal genus Streptochilus from key Neogene marine localities are documented in relation to the evolution of the Gulf of California: S. globigerus, S. latus, S. macdougallae sp. nov., and S. inglei sp. nov. Planktonic foraminiferal bioevents and strontium isotopes in the Bouse, Tirabuzón, Carmen and Ojo de Buey lithostratigraphic units constrain the local distribution range between 6 and 5.3 Ma for the last three species, whereas S. globigerus appears locally at 5.5 Ma and disappears between 3.79 and 3.46 Ma in the Imperial and Trinidad Formations. The last occurrence of Streptochilus latus, and the first and last occurrences of S. globigerus in the ancient Gulf of California are correlated with bioevents calibrated in the equatorial Pacific; therefore, they can be used as reliable local biostratigraphic markers. The presence of Streptochilus in the ancient Gulf of California seems to correlate with upwelling, in a pattern similar to that observed in the modern oceans.

Ordenamiento territorial, turismo y ambiente en Valle de Bravo, México

Directory of Open Access Journals (Sweden)

Nancy Sierra López

2011-01-01

Full Text Available Detrás de ese paisaje idílico de agua, bosques y arquitectura, que la mercadotecnia ofrece y que la tradición evoca, se desarrollaron fuertes conflictos de intereses, necesidades sociales insatisfechas, así como la depredación ambiental constante. En Valle de Bravo pueden observarse paisajes con diferentes visiones y lógicas socioeconómicas, como resultado de un conjunto de políticas de carácter territorial formuladas por el Estado y por la iniciativa privada, con el objetivo de fomentar la actividad turística como eje del desarrollo capitalista. El paisaje creado en algunas zonas ofrece una imagen de prosperidad y confort, mientras que en otras es posible observar la segregación socioterritorial que esta actividad ha generado y que excluye a la mayoría de sus habitantes de los beneficios que el turismo puede traer.

Factores de riesgo que determinan la transmisión de la leishmaniasis en el valle Llaucano, Chota-Cajamarca

Directory of Open Access Journals (Sweden)

Víctor Zorrilla

2005-03-01

Full Text Available Objetivos: Determinar los factores de riesgo asociados con la transmisión de leishmaniasis. Material y Métodos: Se entrevistó 727 personas en 140 viviendas de 8 localidades del valle Llaucano, Chota, Cajamarca. Los factores de riesgo fueron analizados mediante el cálculo del odds ratio, con límites de confianza al 95%, utilizando el pro­grama EpiInfo 2000. Resultados: Se diagnosticó 206 casos de leishmaniasis, 63 lesiones activas y 143 cicatrices. La leishmaniasis se presenta en todos los grupos de edad y ambos sexos están afectados en proporciones similares, siendo más frecuente en menores de 10 años. El alto porcentaje de lesiones en cara y miembros superiores, sugiere una transmisión domiciliaria de la enfermedad. Los factores de riesgo asociados con la transmisión de la leishmaniasis en el valle de Llaucano, son los siguientes: viviendas dispersas ubicadas en áreas rurales (OR 3,97, IC95% 1,94-8,14, dormir en viviendas improvisadas en medio de las chacras en condiciones precarias (OR 4,59, IC95% 3,22-6,54, cultivos de café (OR 7,83, IC95% 3,57-17,17, caña de azúcar (OR 4,99, IC95% 2,42-10,27 y frutas (OR 3,62, IC95% 1,72-7,61 en peridomicilio; hacinamiento con 6 ó más personas por vivienda (OR=3,25, IC95% 1,50-7,10; animales domésticos en el domicilio, principalmente perros (OR=4,03, IC95% 1,98-8,20; flebotominos en el ambiente domiciliario (OR=5,62, IC95% 2,68-11,82, que ingresan a través de las paredes de "tapial". Paccha Baja, Chontabamba y Matibamba son los focos de más alta transmisión de leishmaniasis. La prevalencia acumulada fue de 283,4/1000 hab. Conclusiones: El valle de Llaucano es zona endémica con elevada velocidad de propagación de la leishmaniasis; la transmisión de la enfermedad está asociada a factores de vivienda y comportamiento humano.

Geomorfologické a petrografické aspekty fluviálních sedimentů v oblasti dolní Rokytné

Czech Academy of Sciences Publication Activity Database

Roštínský, Pavel; Šmerda, J.; Nováková, Eva

2016-01-01

Roč. 13, č. 13 (2016), s. 15-58 ISSN 1212-3560 Institutional support: RVO:68145535 Keywords : valley system * fluvial sediments * Boskovická brázda half-graben Subject RIV: DE - Earth Magnetism, Geodesy, Geography OBOR OECD: Geology

Integrated study on the topographic and shallow subsurface expression of the Grote Brogel Fault at the boundary of the Roer Valley Graben, Belgium

Science.gov (United States)

Deckers, Jef; Van Noten, Koen; Schiltz, Marco; Lecocq, Thomas; Vanneste, Kris

2018-01-01

The Grote Brogel Fault (GBF) is a major WNW-ESE striking normal fault in Belgium that diverges westward from the NW-SE striking western border fault system of the Roer Valley Graben. The GBF delimits the topographically higher Campine Block from the subsiding Roer Valley Graben, and is expressed in the Digital Terrain Model (DTM) by relief gradients or scarps. By integrating DTM, Electrical Resistivity Tomography (ERT), Cone Penetration Test (CPT) and borehole data, we studied the Quaternary activity of the GBF and its effects on local hydrogeology. In the shallow subsurface (< 50 m) underneath these scarps, fault splays of the GBF were interpreted on newly acquired ERT profiles at two investigation sites: one on the eastern section and the other on the western section, near the limit of the visible surface trace of the fault. Borehole and CPT data enabled stratigraphic interpretations of the ERT profiles and thereby allowed measuring vertical fault offsets at the base of Pleistocene fluvial deposits of up to 12 m. Groundwater measurements in the boreholes and CPTs indicate that the GBF acts as a hydrologic boundary that prevents groundwater flow from the elevated footwall towards the hangingwall, resulting in hydraulic head differences of up to 12.7 m. For the two investigation sites, the hydraulic head changes correlate with the relief gradient, which in turn correlates with the Quaternary vertical offset of the GBF. ERT profiles at the eastern site also revealed a local soft-linked stepover in the shallow subsurface, which affects groundwater levels in the different fault blocks, and illustrates the complex small-scale geometry of the GBF.

Compte rendu de : La vallée électrique,Foëx E. (photographies) et Broennimann T. (textes), 2006, Paris, InFolio éditions, 164 p., 210 photographies en noir et blanc

OpenAIRE

Buisson, André

2008-01-01

Réunies sous le titre La vallée électrique, 210 photographies en noir et blanc du photographe Emmanuel Foëx illustrent l’architecture industrielle, l’urbanisme et le paysage dans l’Arc alpin. Comme un ouvrage classique, l’album est divisé en trois parties : La centrale, le réseau, le transformateur. L’auteur est parti de l’évidence qu’à travers l’arc alpin, les sillons des vallées sont constellés d’usines consacrées à la fabrication de l’électricité (La centrale). La montagne, telle un châtea...

Neogene vegetation development in the Amazon Basin: evidence from marine well-2, Foz do Amazonas (Brazil)

Science.gov (United States)

Bogota-Angel, Raul; Chemale Junior, Farid; Davila, Roberto; Soares, Emilson; Pinto, Ricardo; Do Carmo, Dermeval; Hoorn, Carina

2014-05-01

Origen and development of the highly diverse Amazon tropical forest has mostly been inferred from continental sites. However, sediment records in the marine Foz do Amazonas Basin can provide important information to better understand the influence of the Andes uplift and climate change on its plant biomes evolution since the Neogene. Sediment analyses of samples from BP-Petrobras well 1 and 2, drilled in the Amazon Fan, allowed to infer the onset of the transcontinental Amazon river and the fan phase during the middle to late Miocene (c. 10.5 Ma). As part of the CLIMAMAZON research programme we performed pollen analysis on the 10.5 to 0.4 Ma time interval. 76 ditch cutting samples of the upper 4165 m sediments of well 2 permitted us to infer changes in floral composition in the Amazon Basin. The palynological spectra across this interval (nannofossil based age model) include pollen, fern spores, dinocysts and foram lignings. When possible pollen and fern spores were grouped in four vegetation types: estuarine, tropical, mountain forest and high mountain open treeless vegetation. Pollen is generally corroded and reflects the effects of sediment transportation while reworked material is also common. Good pollen producers such as Poaceae, Asteraceae and Cyperaceae are common and reflect indistinctive vegetation types particularly those associated to riverine systems. Rhizophora/Zonocostites spp. indicate "close-distance" mangrove development. Tropical forest biomes are represented by pollen that resemble Moraceae-Urticaceae, Melastomataceae-Combretaceae, Sapotaceae, Alchornea, Euphorbiaceae, Rubiaceae, Bignoniaceae, Mauritia and Arecaceae. Myrica, and particularly sporadic occurrences of fossil fern spores like Lophosoria, and Cyathea suggest the development of a moist Andean forest in areas above 1000 m. First indicators of high altitudes appear in the last part of late Miocene with taxa associated to current Valeriana and particularly Polylepis, a neotropical taxon

Resolving the velocity and strain fields in the Upper Rhine Graben Area from a Combination of Levelling, GNSS and InSAR

Science.gov (United States)

Westerhaus, Malte; Fuhrmann, Thomas; Mayer, Michael; Zippelt, Karl; Heck, Bernhard

2016-04-01

The Upper Rhine Graben (URG), located in the tri-national region between Germany, France and Switzerland is the most prominent segment of the European Cenozoic rift system. In recent times, the URG area is characterised by small tectonic movements (less than 1 mm/a) and moderate seismicity up to M=5. Historically, earthquake magnitudes exceeding M=6 have been reported showing that the seismic hazard is quite high. The contemporary tectonic surface deformations are superimposed by displacements caused by anthropogenic activities in various locations in the area, such as coal and potash mining, groundwater usage, oil extraction, geothermal energy and CO2 storage. We use data sets from levelling campaigns, InSAR and permanent GNSS sites to raise an inventory of the current 3D surface displacements and strain rates in the URG with high precision and high spatial resolution. Precise levellings carried out by the surveying authorities of Germany, France and Switzerland since the end of the 19th century have been combined to form a network of levelling lines. A kinematic network adjustment is applied on the levelling data, providing an accurate solution for vertical displacement rates at the levelling benchmarks. InSAR is used to fill gaps in the interior of the levelling loops and to significantly increase the number of points. All the available ERS-1/2 and Envisat scenes from two acquisition geometries covering a period from 1992 to 2000 and 2002 to 2010, resp., are processed according to the Persistent-Scatterer approach. In addition, coordinate time series of 76 permanent sites of the GNSS URG Network are used to support the derivation of the horizontal velocity field of the region. Daily GPS-solutions obtained in differential mode are available since 2004. In a first step, estimates of the surface displacement rates are derived from each technique starting from the raw data. Subsequently, the single-technique deformation estimates are mathematically combined to a 3D

Tectonic geomorphology and volcano-tectonic interaction in the eastern boundary of the Southern Cascades (Hat Creek Graben region, California, USA

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Engielle Mae Raot-raot Paguican

2016-07-01

Full Text Available The eastern boundary of the Southern Cascades (Hat Creek Graben region, California, USA, is an extensively faulted volcanic corridor between the Cascade Range and Modoc Plateau. The east-west extending region is in the transition zone between the convergence and subduction of the Gorda Plate underneath the North American Plate; north-south shortening within the Klamath Mountain region; and transcurrent movement in the Walker Lane. We describe the geomorphological and tectonic features, their alignment and distribution, in order to understand the tectonic geomorphology and volcano-tectonic relationships. One outcome of the work is a more refined morpho-structural description that will affect future hazard assessment in the area.A database of volcanic centers and structures was created from interpretations of topographic models generated from satellite images. Volcanic centers in the region were classified by morphological type into cones, sub-cones, shields and massifs. A second classification by height separated the bigger and smaller edifices and revealed an evolutionary trend. Poisson Nearest Neighbor analysis shows that bigger volcanoes are spatially dispersed while smaller ones are clustered. Using volcano centroid locations, about 90 lineaments consisting of at least three centers within 6km of one another were found, revealing that preferential north-northwest directed pathways control the transport of magma from the source to the surface, consistent with the strikes of the major fault systems. Most of the volcano crater openings are perpendicular to the maximum horizontal stress, expected for extensional environments with dominant normal regional faults. These results imply that the extension of the Hat Creek Graben region and impingement of the Walker Lane is accommodated mostly by extensional faults and partly by the intrusions that formed the volcanoes. Early in the history of a volcano or volcano cluster, melt produced at depth in the

Estudio preliminar de la fauna Amphibia del valle de Sibundoy, Alto Putumayo, Colombia

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Jonh Jairo Mueses-Cisneros

2004-07-01

(Valle de Sibundoy y por localidades muestreadas, se hace una comparación con las faunas realizadas en el transecto Napo en Ecuador y en el transecto Montañita-Alto Gabinete en Caquetá y se presenta una clave taxonómica y una serie de fotografías para facilitar su  reconocimiento. El estudio además aporta cinco especies nuevas para la ciencia, amplía el rango altitudinal de otras ocho y presenta tres más para ser incluidas al listado general de las especies de anfibios de Colombia, las cuales habían sido ya anteriormente reportadas para el país por otros autores, pero no habían sido tenidas en cuenta en el último listado.

A review of the sedimentology of the Early Proterozoic Pretoria Group, Transvaal Sequence, South Africa: implications for tectonic setting

Science.gov (United States)

Eriksson, P. G.; Schreiber, U. M.; van der Neut, M.

The sedimentary rocks of the Early Proterozoic Pretoria Group form the floor rocks to teh 2050 M.a. Bushveld Complex. An overall alluvial fan-fan-delta - lacustrine palaeoenvironmental model is postulated for the Pretoria Group. This model is compatible with a continental half-graben tectonic setting, with steep footwall scarps on the southern margin and a lower gradient hanging wall developed to the north. The latter provided much of the basin-fill detritus. It is envisaged that the southern boundary fault system migrated southwards by footwall collapse as sedimentation continued. Synsedimentary mechanical rifting, associated with alluvial and deltaic sedimentation (Rooihoogte-Strubenkop Formations) was followed by thermal subsidence, with concomitant transgressive lacustrine deposition (Daspoort-Magaliesberg Formations). The proposed half-graben basin was probably related to the long-lived Thabazimbi-Murchison and Sugarbush-Barberton lineaments, which bound the preserved outcrops of the Pretoria Group.

Acceso a la tierra de los ex huasipungueros en la hacienda "Carpuela", en el valle del Chota.

OpenAIRE

Villa Zura, Marco Patricio

2015-01-01

El propo?sito del presente estudio de investigacio?n es abordar como fue el acceso a la tierra de los ex huasipungueros en la hacienda Carpuela en el Valle del Chota, parroquia Ambuqui?, canto?n Ibarra, Provincia de Imbabura, quienes fortalecieron la organizacio?n comunitaria, apoya?ndose en la Ley de Reforma Agraria, ejecutada por el Instituto Ecuatoriano de Reforma Agraria y Colonizacio?n de 1964 y la de 1973 que continuo. Adema?s autores teo?ricos reflejan la historia de los jesuitas qu...

Writing on the Edge: Impressions of a U.S.-Mexico Border in Rolando Hinojosa's Estampas del Valle

OpenAIRE

CANTU, MARIA GUADALUPE

2011-01-01

This dissertation engages in a critical reading of Rolando Hinojosa's early fiction in Estampas del Valle as an example of a unique border literature that highlights the multiplicity of elements that exist along the Rio Grande. By using the work of an author that has direct experience with life along the U.S.-Mexico border the aim of this study is to look at how the border region and its cultural and spatial manifestations impact on writings concerned with memory, the personal and the self. ...

El Paleolítico Medio en el Cáucaso Meridional: la Cueva Doble (Valle de Tsutskhvati, República de Georgia

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Fernando DÍEZ MARTÍN

2010-08-01

Full Text Available El presente trabajo recoge los principales resultados derivados de la intervención arqueológica acometida entre los años 2002 y 2003 en el Valle de Tsutskhvati (República de Georgia, principalmente centrados en una nueva ronda de excavaciones en la Cueva Doble. Los estudios estratigráficos, tecnológicos, tafonómicos y polínicos permiten arrojar nuevos datos, complementarios a los obtenidos en la cercana cueva de Ortvale Klde, sobre las comunidades neandertales que habitaron la región del Cáucaso meridional, uno de los entornos geográficos en los que sobrevivieron los últimos representantes de esta especie. Mientras que los completos trabajos arqueológicos abordados en la cueva de Ortvale Klde han permitido contar con un amplio programa de datación para la presencia neandertal en dicha cavidad, el resto de los yacimientos del mismo periodo siguen presentando una cierta indefinición contextual. A pesar de ello, se acepta que la presencia neandertal en el valle de Tsutskhvati debió situarse en el mismo marco temporal que en Ortvale Klde. Aunque tanto la Cueva Doble, motivo de esta publicación, como la famosa Cueva del Bronce carecen hoy en día de contextos cronológicos fiables, es necesario señalar que estos yacimientos del valle de Tsutskhvati vienen siendo recurrentemente citados en el debate sobre el fin de los neandertales y la llegada de las primeras comunidades sapiens a la región caucásica. Es por ello por lo que la información novedosa aquí presentada (los últimos trabajos en Tsutskhvati se llevaron a cabo en la década de 1970 posee un indudable interés, a pesar de las limitaciones cronológicas, para ampliar nuestro conocimiento sobre este importante capítulo de la Prehistoria europea.

Mechanical conditions and modes of paraglacial deep-seated gravitational spreading in Valles Marineris, Mars

Science.gov (United States)

Makowska, Magdalena; Mège, Daniel; Gueydan, Frédéric; Chéry, Jean

2016-09-01

Deep-seated gravitational spreading (DSGS) affects the slopes of formerly glaciated mountain ridges. On Mars, DSGS has played a key role in shaping the landforms of the giant Valles Marineris troughs. Though less spectacular, DSGS is common in terrestrial orogens, where understanding its mechanics is critical in the light of the ongoing climate change because it is a potential source of catastrophic landslides in deglaciated valleys. We conducted parametric numerical studies in order to identify important factors responsible for DSGS initiation. DSGS models are computed using an elastoviscoplastic finite element code. Using ADELI's software, we reproduce topographic ridge spreading under the effect of valley unloading. Two types of spreading topographic ridges are investigated, homogeneous or with horizontal rheological layering. We find that gravitational instabilities are enhanced by high slopes, which increase gravitational stress, and low friction and cohesion, which decrease yield stress. In the unlayered ridge, instability is triggered by glacial unloading with plastic strain concentration inside the ridge and at the base of the high slopes. Vertical fractures develop in the upper part of the slope, potentially leading to fault scarps. Ridge homogeneity promotes a deformation mode controlled by uphill-facing normal faulting and basal bulging. In the second case, the ridge encompasses horizontal geological discontinuities that induce rock mass anisotropy. Discontinuity located at the base of the slope accumulates plastic strain, leading to the formation of a sliding plane evolving into a landslide. The presence of a weak layer at ridge base therefore promotes another slope deformation mode ending up with catastrophic failure. Mechanical conditions and slope height being equal, these conclusions can probably be extrapolated to Earth. Compared with Mars, DSGS on Earth is inhibited because terrestrial topographic gradients are lower than in Valles Marineris, an

Bienestar y participación, una construcción local. Versalles, Valle del Cauca

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Mark Lundy

1999-01-01

Full Text Available El concepto de desarrollo local se ha venido construyendo tanto en el escenario académico como en los diferentes espacios de trabajo comunitario existentes en Colombia. El presente artículo retoma una de estas experiencias, la del Comité de Participación Comunitaria del municipio de Versalles, Valle del Cauca, y la desglosa por medio de una descripción, el análisis de los logros y algunas reflexiones acerca de lo vivido. El ejercicio permite avanzar en la definición de algunos conceptos, clarificar retos futuros, proponer algunos pasos necesarios para potenciar el desarrollo humano e identificar ciertas variables claves en el proceso de desarrollo local.

Valles Marineris as a Cryokarstic Structure Formed by a Giant Dyke System: Support From New Analogue Experiments

Science.gov (United States)

Ozeren, M. S.; Sengor, A. M. C.; Acar, D.; Ülgen, S. C.; Onsel, I. E.

2014-12-01

Valles Marineris is the most significant near-linear depression on Mars. It is some 4000 km long, up to about 200 km wide and some 7 km deep. Although its margins look parallel at first sight, the entire structure has a long spindle shape with significant enlargement in its middle (Melas Chasma) caused by cuspate slope retreat mechanisms. Farther to its north is Hebes Chasma which is an entirely closed depression with a more pronounced spindle shape. Tithonium Chasma is a parallel, but much narrower depression to its northeast. All these chasmae have axes parallel with one another and such structures occur nowhere else on Mars. A scabland surface exists to the east of the Valles Marineris and the causative water mass seems to have issued from it. The great resemblance of these chasmae on mars to poljes in the karstic regions on earth have led us to assume that they owed their existence to dissolution of rock layers underlying them. We assumed that the dissolving layer consisted of water ice forming substantial layers, in fact entirely frozen seas of several km depth. We have simulated this geometry by using bentonite and flour layers (in different experiments) overlying layers of ice in which a resistant coil was used to simulate a dyke. We used different thicknesses of bentonite and flour overlying ice layers again of various thicknesses. The flour seems to simulate the Martian crust better because on Mars, g is only about 3/8ths of its value on Earth, so (for equal crustal density) the depth to which the cohesion term C remains important in the Mohr-Coulomb shear failure criterion is about 8/3 times greater. As examples we show two of those experiments in which both the rock analogue and ice layers were of 1.5 cm. thick. Perfect analogues of the Valles Marineris formed above the dyke analogue thermal source complete with the near-linear structure, overall flat spindle shape, cuspate margins, a central ridge, parallel side faults, parallel depressions resembling

Vacancy induced half-metallicity in half-Heusler semiconductors

KAUST Repository

Zhu, Zhiyong

2011-09-28

First-principles calculations are performed to investigate the effect of vacancies on the electronic structure and magnetic properties of the two prototypical half-Heusler semiconductors NiTiSn and CoTiSb. The spin degeneracy of the host materials is broken for all types of isolated vacancies under consideration, except for Ni-deficient NiTiSn. A half-metallic character is identified in Sn-deficient NiTiSn and Co/Ti/Sb-deficient CoTiSb. We can explain our findings by introducing an extending Slater-Pauling rule for systems with defects. A ferromagnetic ordering of the local moments due to double exchange appears to be likely.

Mapping Neogene and Quaternary sedimentary deposits in northeastern Brazil by integrating geophysics, remote sensing and geological field data

Science.gov (United States)

Andrades-Filho, Clódis de Oliveira; Rossetti, Dilce de Fátima; Bezerra, Francisco Hilario Rego; Medeiros, Walter Eugênio; Valeriano, Márcio de Morisson; Cremon, Édipo Henrique; Oliveira, Roberto Gusmão de

2014-12-01

Neogene and late Quaternary sedimentary deposits corresponding respectively to the Barreiras Formation and Post-Barreiras Sediments are abundant along the Brazilian coast. Such deposits are valuable for reconstructing sea level fluctuations and recording tectonic reactivation along the passive margin of South America. Despite this relevance, much effort remains to be invested in discriminating these units in their various areas of occurrence. The main objective of this work is to develop and test a new methodology for semi-automated mapping of Neogene and late Quaternary sedimentary deposits in northeastern Brazil integrating geophysical and remote sensing data. The central onshore Paraíba Basin was selected due to the recent availability of a detailed map based on the integration of surface and subsurface geological data. We used airborne gamma-ray spectrometry (i.e., potassium-K and thorium-Th concentration) and morphometric data (i.e., relief-dissection, slope and elevation) extracted from the digital elevation model (DEM) generated by the Shuttle Radar Topography Mission (SRTM). The procedures included: (a) data integration using geographic information systems (GIS); (b) exploratory statistical analyses, including the definition of parameters and thresholds for class discrimination for a set of sample plots; and (c) development and application of a decision-tree classification. Data validation was based on: (i) statistical analysis of geochemical and airborne gamma-ray spectrometry data consisting of K and Th concentrations; and (ii) map validation with the support of a confusion matrix, overall accuracy, as well as quantity disagreement and allocation disagreement for accuracy assessment based on field points. The concentration of K successfully separated the sedimentary units of the basin from Precambrian basement rocks. The relief-dissection morphometric variable allowed the discrimination between the Barreiras Formation and the Post-Barreiras Sediments. In

Role of Neogene Exhumation and Sedimentation on Critical-Wedge Kinematics in the Zagros Orogenic Belt, Northeastern Iraq, Kurdistan

Science.gov (United States)

Koshnaw, R. I.; Horton, B. K.; Stockli, D. F.; Barber, D. E.; Tamar-Agha, M. Y.; Kendall, J. J.

2014-12-01

The Zagros orogenic belt and foreland basin formed during the Cenozoic Arabia-Eurasia collision, but the precise histories of shortening and sediment accumulation remain ambiguous, especially at the NW extent of the fold-thrust belt in Iraqi Kurdistan. This region is characterized by well-preserved successions of Cenozoic clastic foreland-basin fill and deformed Paleozoic-Mesozoic hinterland bedrock. The study area provides an excellent opportunity to investigate the linkage between orogenic wedge behavior and surface processes of erosion and deposition. The aim of this research is to test whether the Zagros orogenic wedge advanced steadily under critical to supercritical wedge conditions involving in-sequence thrusting with minimal erosion or propagated intermittently under subcritical condition involving out-of-sequence deformation with intense erosion. These endmember modes of mountain building can be assessed by integrating geo/thermochronologic and basin analyses techniques, including apatite (U-Th)/He thermochronology, detrital zircon U-Pb geochronology, stratigraphic synthesis, and seismic interpretations. Preliminary apatite (U-Th)/He data indicate activation of the Main Zagros Fault (MZF) at ~10 Ma with frontal thrusts initiating at ~8 Ma. However, thermochronometric results from the intervening Mountain Front Flexure (MFF), located between the MZF and the frontal thrusts, suggest rapid exhumation at ~6 Ma. These results suggest that the MFF, represented by the thrust-cored Qaradagh anticline, represents a major episode of out-of-sequence deformation. Detrital zircon U-Pb analyses from the Neogene foreland-basin deposits show continuous sediment derivation from sources to the NNE in Iraq and western Iran, suggesting that out-of-sequence thrusting did not significantly alter sedimentary provenance. Rather, intense hinterland erosion and recycling of older foreland-basin fill dominated sediment delivery to the basin. The irregular distribution of

Movilidad y dieta en el valle de El Mauro (31° 57’ S. - 71° 01’ W.), Norte Semiárido de Chile, entre 8350-929 CAL. AP

OpenAIRE

Gómez, Pablo; Pacheco, Aryel

2016-01-01

El valle de El Mauro se localiza a 40 km del Océano Pacífico (1000 msnm) en el extremo meridional del Norte Semiárido de Chile. Para contribuir al conocimiento de la movilidad y dieta prehispánica en el valle se analizó el radiocarbono y los isótopos de estroncio (87Sr/86Sr), oxígeno (δ¹13O), nitrógeno (δ¹13N) y carbono (δ13C) de 21 individuos y un entierro múltiple (NMI=3).Los datos indican el arribo esporádico de individuos de origen y/o hábitat costeros entre 8350-3000 cal. AP. Posterior a...

El poblamiento humano antiguo en el valle alto del Lozoya (Madrid

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Belén Márquez

2008-01-01

Full Text Available La localización en superficie en el término municipal de Lozoya (Madrid de un conjunto de piezas de industria lítica achelense permite retrotraer el primer poblamiento de esta zona al Pleistoceno medio, cuando hasta la fecha las evidencias más antiguas en el valle alto del río Lozoya se remontaban a inicios del Pleistoceno superior. El nuevo hallazgo sitúa al río Lozoya en relación cultural con el poblamiento humano antiguo de los ríos Jarama y Manzanares.The discovery of a surface sample of Acheulean lithic industry at the Lozoya district (Madrid takes back to the Middle Pleistocene the first human peopling of this area. Until now themost ancient evidences at the Upper Lozoya Valley went back to the initial Upper Pleistocene. The new findings place the Lozoya River in cultural relation with the ancient human population of Jarama and Manzanares Rivers.

Incidencia del fenómeno ENSO en la hidroclimatología del valle del río Cauca-Colombia

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1998-01-01

Full Text Available IMPACT DU PHÉNOMÈNE ENSO SUR L’HYDROCLIMATOLOGIE DU RIO CAUCA-COLOMBIE. On présente dans cet article quelques unes des manifestations du phénomène et leur impact sur la pénurie des ressources en eau dans la vallée du rio Cauca, au cours des périodes sèches ainsi que les crues et inondations, provoquées par les périodes excédentaires. L’évaluation de valeurs extrêmes des débits des rivières montre des différences liées à l’occurrence d’un El Niño. En présence d’un El Niño, les débits maximums seront plus forts et les débits d’étiages plus faibles. Au cours de ces périodes, on observe donc une augmentation du risque d’inondation au cours de la saison des pluies, alors que la quantité d’eau diminue au cours des périodes sèches avec un risque accru d’incendie de forêt. En este trabajo, se presentan algunas de las manifestaciones del Fenómeno y el impacto que ocasiona en la disponibilidad hídrica del Valle del Cauca durante la fase Cálida (Niño, por efecto del déficit hídrico, y durante la fase fría (AntiNiño o Niña por exceso de lluvias. La evaluación de los caudales mínimos de los ríos del Valle del Río Cauca, se asocia con los años de ocurrencia de la fase cálida, mientras los caudales medios máximos se asocian a períodos de ocurrencia de la fase fría (AntiNiño o Niña. Durante el Niño se presentan sequías, incendios forestales, pérdidas de cultivos, de perecederos, disminución de la pesca, incremento de enfermedades y racionamiento de energía, mientras que durante la Niña se presentan mayores riesgos de inundación, desbordamientos, desastres, erosión y destrucción de la infraestructura vial e hidráulica. INCIDENCE OF ENSO PHENOMENON IN THE HYDROCLIMATOLOGY OF THE RÍO CAUCA VALLEY-COLOMBIA. In this paper, the impacts of the El Niño and La Niña o AntiNiño phenomena on the water resources of the Valle del Cauca (Colombia are considered low flows in the rivers are associated with

Australian Northwest Shelf: a Late Neogene Reversible Tectonic Event

Science.gov (United States)

Kominz, M. A.; Gurnis, M.; Gallagher, S. J.; Expedition 356 Scientists, I.

2017-12-01

The Northwest Shelf (NWS) of Australia is characterized by several offshore basins with active rifting in Permian and Jurassic time. Thus, by the Late Neogene this continental margin should be a very slowly subsiding passive margin. However, thick, poorly dated sediments have been noted in this region leading to speculation that this part of Australia has undergone down-warping in this time period. The International Ocean Discovery Program (IODP) Expedition 356 was designed, in part, to better constrain this even in both time and space. Post-cruise Airy-backstripping analyses of samples from four IODP 356 well sites, located as far south as the Perth Basin and as far North as the Carnarvon Basin, suggest that, in fact, this region has undergone a latest Miocene (≈ 8 to 6 Ma) subsidence event followed by a later (≈ 2 to 1 Ma) uplift event. Age constraints are from micropaleontology with some refinement using climate cycle-stratigraphy. Water depth constraints are from benthic foraminifera and from quantitative ratios of benthic foraminifera to planktonic foraminifera. These event cannot be explained as related to either the high-magnitude glacial eustatic changes nor can the uplift event be eliminated and ascribed to sediments filling the accommodation space generated in the earlier event. The magnitude and duration of the vertical movements are remarkably similar and suggests that the subsidence is reversible. Reversibility is a key aspect of a dynamic topography signal. However, it is difficult to produce a mantle anomaly that reproduces the subsidence and subsequent uplift with the requisite amplitude and rates as observed in the NWS of Australia. Additionally, the subduction of the Australian Plate into the Java Trench is too distant to affect this region of Australia. Modeling of a flexural warping due to in-plane stress related to collision of Timor with the Java trench is

Trabajo Multidisciplinar Universidad-Empresa en Agroindustria Cafetera del Valle del Cauca, Colombia Multidisciplinary Collaboration University-Industry in a Coffee Growing Enterprise of Valle del Cauca, Colombia

Directory of Open Access Journals (Sweden)

Jaime A. Aguilar Zambrano

2009-12-01

Full Text Available Este artículo presenta una metodología y los resultados obtenidos de un proyecto de actuación multidisciplinar en una relación universidad-empresa para favorecer la innovación. Desde la universidad participaron profesores y estudiantes de los Programas de Ingeniería Electrónica e Ingeniería Industrial, y la empresa fue una cooperativa de cultivadores de café orgánico llamada Asociación ACOC, ubicada en el centro del Valle del Cauca en Colombia. Se plantearon dos hipótesis para el proyecto, la primera: el trabajo multidisciplinar genera mejores resultados en la solución de problemas de las pequeñas empresas porque contempla el problema en una forma sistémica; la segunda: el trabajo independiente de cada disciplina una vez identificada la problemática técnica provee resultados satisfactorios para el conjunto del problema. La primera hipótesis fue verificada y la segunda se verificó parcialmente. Se concluye que las relaciones universidad-empresa con un aporte tecnológico multidisciplinar mejoran significativamente el trabajo de la pequeña empresa. La empresa debe involucrarse de manera activa para que los resultados perduren en el tiempo y la visión sistémica de los problemas fortalece el trabajo de las pequeñas empresas.This article shows a methodology and the results obtained from a multidisciplinary project between the University and Enterprise which encourages innovation. The University participated with its faculty members and students enrolled in the programs of industrial engineering and electronic engineering, and the Enterprise was a group of organic coffee farmers (called by its founders Asociación ACOC located in the center of Valle del Cauca, Colombia. Two hypotheses were formulated for the project. The first, multidisciplinary work produces better results in solving problems of small businesses because it considers the problem in a systemic way. The second, independent work from each field of study, once the

Las diócesis del Valle del Cauca (Colombia en el siglo XX: Hacia el fortalecimiento de la modernización

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Antonio José Echeverry Pérez

2014-07-01

Full Text Available El presente artículo hace un recorrido histórico (consultando fundamentalmente los archivos diocesanos, en su mayoría inéditos, por la instauración de las principales diócesis creadas en el Departamento del Valle del Cauca (Colombia durante el siglo XX: Cali, Palmira, Buenaventura, Cartago y Buga. Se muestra como la Iglesia constituye un proyecto fundamental de modernización religiosa, que se denota ante todo en la extensión de su presencia en el territorio vallecaucano. Proceso que inicia con la desfragmentación del gran territorio de la arquidiócesis de Popayán, con lo cual cada diócesis creada logra impulsar sus propios procesos de generación de parroquias, centros educativos y de beneficencia, logrando con esto, construir la iglesia vallecaucana y fortalecer la religión católica tanto en los sectores rurales como en los espacios urbanos del departamento del Valle del Cauca. Cada nueva diócesis se inscribe además, en su propia coyuntura local de desarrollo y modernización económica y social.

Studying disability and disability studies: shifting paradigms of LDA synthesis of responses to Reid and Valle.

Science.gov (United States)

Connor, David J

2005-01-01

In this article, I discuss the 11 diverse responses to Reid and Valle's work on the discursive practice of learning disabilities (LD), implications for instruction, and parent-school relations. I highlight key ideas from each article and then focus on three common areas of interest shared by most respondents: the unacceptable status quo of schooling practices; desired changes in schooling practices; and knowledge production in the field of special education and its relation to schooling practices. In light of the many issues raised, I urge the need for a reflective turn in the field of LD and for openness toward diversification of thought.

Surface half-metallicity of half-Heusler compound FeCrSe and interface half-metallicity of FeCrSe/GaP

Energy Technology Data Exchange (ETDEWEB)

Khalaf Al-zyadi, Jabbar M., E-mail: jabbar_alzyadi@yahoo.com [Department of Physics, College of Education for Pure Sciences, University of Basrah (Iraq); Jolan, Mudhahir H. [Department of Physics, College of Education for Pure Sciences, University of Basrah (Iraq); Yao, Kai-Lun, E-mail: klyao@mail.hust.edu.cn [School of Physics and Wuhan National High Magnetic Field Center, Huazhong University of Science and Technology, Wuhan 430074 (China); International Center of Materials Physics, Chinese Academy of Sciences, Shenyang 110015 (China)

2016-04-01

Recent studies showed that half-Heusler FeCrSe exhibits half-metallic ferromagnetism (Huang et al. [20]). In this paper, we investigate extensively the electronic, magnetic, and half-metallic properties of the half-Heusler alloy FeCrSe (111) and (001) surfaces and the interface with GaP (111) substrate by using the first-principles calculations within the density functional theory. The atomic density of states demonstrates that the half-me tallicity verified in the bulk FeCrSe is maintained at the CrSe-terminated (001) and Se-terminated (111) surfaces, but lost at both Cr- and Fe-terminated (111) surfaces and the Fe-terminated (001) surface. Alternatively, for the interface of FeCrSe/GaP (111), the bulk half-metallicity is destroyed at Se–P configuration while Se–Ga interface and subinterface show nearly 100% spin polarization. Moreover, the calculated interfacial adhesion energies exhibit that Se–Ga shape is more stable than the Se–P one. The calculated magnetic moments of Se, Ga at the Se–Ga (111) interface and P at the Se–P (111) interface increase with respect to the corresponding bulk values while the atomic magnetic moment of Se atom at the Se–P (111) interface decreases. We also notice that the magnetic moments of subinterface Fe at both Se–Ga and Se–P (111) interfaces decrease compared to the bulk values. - Highlights: • The half-metallicity verified in the bulk FeCrSe is kept at the CrSe-terminated (001) and Se-terminated (111) surfaces. • The calculated interfacial adhesion energies exhibit that Se–Ga shape is more stable than Se–P. • The magnetic moments of Se, Ga and P atoms at the interface increase. • The Se–Ga interface shows nearly 100% spin polarization.

Efecto de la calidad de agua del acuífero Valle de Guadalupe en la salinidad de suelos agrícolas Water quality effect on the Valle de Guadalupe aquifer in the agricultural soils salinity

OpenAIRE

Jorge Arturo Salgado Tránsito; Oscar Palacios Vélez; Arturo Galvis Spínola; Francisco Gavi Reyes; Enrique Mejía Sáenz

2012-01-01

Para determinar el efecto de la calidad del agua en el Acuífero del Valle de Guadalupe, Baja California, México, en la salinidad de los suelos agrícolas se midió el pH, conductividad eléctrica, sólidos disueltos totales y la concentración de los principales iones en las aguas de 66 pozos, de un total de 754 que se encontraban en operación en el acuífero durante 2009 .Y se analizó en el extracto de pasta de saturación de muestras de suelo el pH, conductividad eléctrica, carbonato, bicarbonato,...

Spatiotemporal Effects of Climate Variability and Urban Growth on the "Valle de Toluca" Aquifer (Mexico)

Science.gov (United States)

Mastachi-Loza, C. A.; Diaz-Delgado, C.; Esteller, M. V.; Gomez-Albores, M. A.; Becerril, R.; Ruiz-Gomez, M. D.

2013-05-01

Toluca city is located in the "Valle de Toluca" at the upper course of the Lerma river basin, is an important economic center which contributes with 1.2% of Gross National Product (GNP) since it is an industrial city, The city has grown due to the economic development sustained by the "Valle de Toluca" aquifer which provides water for human consumption, industrial facilities and crop irrigation. Recent studies have shown that in the last 50 years the annual precipitation rate in Toluca has increased 122 mm, whereas the daily minimum temperature has increased 1.1 °C and the daily maximum temperature has also increased 0.8 °C. These results show a general overview of the change in the climate conditions of the city; however they do not show the spatial distribution of the change. For this reason, the aim of this work was to evaluate the spatiotemporal change of precipitation rates and urban growth in order to determine their effects over the "Valle de Toluca" aquifer. In order to detect the urban growth, a supervised classification technique has been used taking into account Landsat TM satellite images between 1973, 1986, 2000 and 2005. A yearly spatiotemporal raster set of rainfall rates from 1980 to 2010 were obtained interpolating data from 812 climatologic stations. To evaluate the effect in annual precipitation rates and urban growth over the aquifer, we interpolate data from 38 piezometers from 1980 to 2010 to obtain a spatiotemporal raster set. The piezometric values correspond to the aquifer's upper level. The spatiotemporal raster sets were analyzed with the non-parametric Theil-Sen test to determine trends in piezometric levels and precipitation rates. Finally the urban growth, spatial-temporal trends of precipitation rates and piezometric levels were displayed in a GIS and then subjectively analyzed to figure out coincidences. An increase in annual precipitation rates (+87 mm) over Toluca's Valley during the last three decades was observed specially

Le aree rurali dell’Appennino Ligure tra età romana e tardomedioevo. Ricerche storiche e archeologiche in alta Valle Scrivia / The rural areas of the Ligurian Appennines between Roman period and the Late Middle Ages. Historical and archaeological research in Valle Scrivia

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Giovanni Battista Parodi

2015-12-01

Full Text Available La ricerca è incentrata sull’analisi delle forme e delle dinamiche del popolamento, delle strutture e dell’organizzazione del territorio dell’alta Valle Scrivia (area appenninica ubicata tra Genova e la pianura che mai è stata oggetto di ricerche sistematiche tra la tarda antichità e il XV secolo, alla luce delle fonti storiche, cartografiche e archeologiche. In particolare, la realizzazione di indagini di superficie e shovel tests ha consentito di ampliare e approfondire la conoscenza del comprensorio nel periodo in esame, fornendo interessanti spunti per lo studio delle aree rurali appenniniche. Gli elementi raccolti sono confl uiti all’interno di un database e di una piattaforma GIS appositamente creata. The research focuses on the analysis of settlement forms and dynamics, structures and organisation of upper Valle Scrivia (an area in the Apennines located between Genoa and the Po Valley that has never been the object of systematic studies between Late Antiquity and the 15th century in light of historical, cartographic and archaeological sources. In particular, carrying out surface surveys and shovel tests allowed to widen and increase the knowledge of the area in the period examined and provided interesting ideas for the study of rural areas in the Apennines. The elements that were gathered were inserted into a database and a GIS platform created on purpose.

Syndrome of the caregiver in disability old patients and the psychosocial implications. Valle del Cauca, Colombia 2003-2004.

OpenAIRE

Eliana Dueñas; María Anggeline Martínez; Benjamín Morales; Claudia Muñoz; Ana Sofía Viáfara; Julián A. Herrera

2009-01-01

Objetivo: Describir la prevalencia del síndrome del cuidador y las características psicosociales de los cuidadores de adultos mayores discapacitados. Materiales y métodos: Se realizó un estudio piloto de casos y controles en el Valle del Cauca durante el 2003-2004 para evaluar la funcionalidad familiar (APGAR familiar), la ansiedad y depresión (escala de Goldberg), la presencia de enfermedades (cuidadores y no cuidadores), y la prevalencia del síndrome del cuidador (escala de Zarit). Resultad...

INTER-DIDÁCTICA -El reto intercultural del maestro inmigrante en el Valle del Guamuéz (Putumayo, Colombia)-

OpenAIRE

Armero Díaz, Amanda Milena; Enríquez López, Miriam Fernanda; Osejo Ortega, Myrian Patricia; Betancourth Nastul, Wilson

2016-01-01

Tesis (Maestría en Educación desde la Diversidad). Universidad de Manizales. Facultad de Ciencias Sociales y Humanas, 2015 Los procesos de enseñanza-aprendizaje, a la vanguardia post-moderna, ameritan asumir una nueva perspectiva de la didáctica, demostrando en esta investigación que el componente cultural juega un papel trascendental en su transformación. El siguiente estudio surge de la premisa investigativa ¿Cómo fortalecer la identidad cultural del Valle del Guamuéz, Departam...

Las necesidades de capacitación de empresarios de MIPYMES del Valle de Mexicali, México, y la demanda de capacitación de los mismos, en el semestre 2011-1

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Marcela Reyes Pazos

2012-07-01

Full Text Available El propósito de la investigación es analizar las necesidades de capacitación de empresarios de MIPYMES (Micro, Pequeñas y Medianas Empresas del Valle de Mexicali, y la demanda de capacitación de los mismos, durante el semestre 2011-1. Esta investigación la realiza el cedem-uabc (Centro Desarrollo Empresarial de la Escuela de Ingeniería y Negocios, Guadalupe Victoria, de la Universidad Autónoma de Baja California, campus Mexicali. El método seguido fue investigación cuantitativa, con una muestra aleatoria no representativa de 469 MIPYMES encuestadas de los distintos ejidos del Valle de Mexicali. Los principales resultados obtenidos manifiestan que existe demanda de capacitación, en áreas como administración, publicidad y mercadotecnia, y ventas. Los resultados del diagnóstico de la investigación indican que sí están presentes las necesidades de capacitación por parte de la mayoría de los empresarios de las MIPYMES del Valle de Mexicali, pero muy pocos la han solicitado. Los objetivos de la investigación se lograron analizando las necesidades de capacitación y la demanda de capacitación de los empresarios.

Las necesidades de capacitación de empresarios de MIPYMES del Valle de Mexicali, México, y la demanda de capacitación de los mismos, en el semestre 2011-1

Directory of Open Access Journals (Sweden)

Marcela Reyes Pazos

2012-06-01

Full Text Available El propósito de la investigación es analizar las necesidades de capacitación de empresarios de MIPYMES (Micro, Pequeñas y Medianas Empresas del Valle de Mexicali, y la demanda de capacitación de los mismos, durante el semestre 2011-1. Esta investigación la realiza el cedem-uabc (Centro Desarrollo Empresarial de la Escuela de Ingeniería y Negocios, Guadalupe Victoria, de la Universidad Autónoma de Baja California, campus Mexicali. El método seguido fue investigación cuantitativa, con una muestra aleatoria no representativa de 469 MIPYMES encuestadas de los distintos ejidos del Valle de Mexicali. Los principales resultados obtenidos manifiestan que existe demanda de capacitación, en áreas como administración, publicidad y mercadotecnia, y ventas. Los resultados del diagnóstico de la investigación indican que sí están presentes las necesidades de capacitación por parte de la mayoría de los empresarios de las MIPYMES del Valle de Mexicali, pero muy pocos la han solicitado. Los objetivos de la investigación se lograron analizando las necesidades de capacitación y la demanda de capacitación de los empresarios.

Progress Report Phase I: Use, access, and fire/fuels management attitudes and preferences of user groups concerning the Valles Caldera National Preserve (VCNP) and adjacent areas

Science.gov (United States)

Kurt F. Anschuetz; Carol B. Raish

2010-01-01

This document represents a progress report of activities completed during Phase I of the study titled, Use, Access, and Fire/Fuels Management Attitudes and Preferences of User Groups Concerning the Valles Caldera National Preserve (VCNP) and Adjacent Areas, and the preliminary findings of this work.

Un plan de gestión para la prevención y control de la contaminación del aire por BTX (Benceno, Tolueno, Xileno) en el Área Metropolitana del Valle de Aburrá

OpenAIRE

Rubiano Hernández, Claudia Marcela

2013-01-01

Resumen: El presente trabajo desarrolla un plan de gestión para la prevención y control de la contaminación del aire por BTX (Benceno, Tolueno, Xileno) en el área metropolitana del Valle de Aburrá, el cual se considera necesario de acuerdo a los valores obtenidos en las campañas de caracterización realizadas en las zonas urbanas del valle y que evidencian niveles que sobrepasan la norma en algunos puntos de muestreo poniendo en riesgo a mediano y largo plazo la salud de los habitantes de la r...

Neogene basin infilling from cosmogenic nuclides (10Be and 21Ne) in Atacama, Chile

Science.gov (United States)

Sanchez, Caroline; Regard, Vincent; Carretier, Sébastien; Riquelme, Rodrigo; Blard, Pierre-Henri; Campos, Eduardo; Brichau, Stéphanie; Lupker, Marteen; Hérail, Gérard

2017-04-01

In the hyperarid Atacama Desert, northern Chile, Neogene sediments host copper rich layers (exotic supergene mineralization). Current mines are excavated into relatively thin (production (quickly decreasing with depth) and disintegration (not for 21Ne). Sampling depths are at ˜100 m and at ˜50 m below the desert surface. First, 21Ne gives lower boundaries for upstream erosion rates or local sedimentation rate. These bounds are between 2 and 10 m/Ma, which is quite important for the area. The ratio between the two cosmogenic nuclides indicate a maximum burial age of 12 Ma (minimal erosion rate of 15 m/Ma) and is surprisingly similar from bottom to top, indicating a probable rapid infilling. We finally processed a Monte-Carlo inversion. This inversion helps taking into account the post-deposition muonic production of cosmogenic nuclides. Inversion results is dependent on the muonic production scheme. Interestingly, the similarity in concentrations from bottom to top pleads for quite low production at depth. Our data finally indicates a quick infilling between 12.5 and 10 Ma BP accounting for ˜100 m of deposition (minimum sedimentation rate of 40 m/Ma).

First record of Annonaceae wood for the Neogene of South America, Amazon Basin, Brazil

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Emilio Alberto Amaral Soares

Full Text Available ABSTRACT: The relief of the regions of Manaus and Itacoatiara, Central Amazon, is supported by Neogene siliciclastic rocks, bounded at the base and top by lateritic paleosols and covered by quaternary sedimentary deposits from the Solimões-Amazon river system. This unit is informally assigned to the Novo Remanso Formation, consists of usually reddish and ferruginized sandstones, conglomerates and pelites, with few identified fossil records, a fact that has hindered its stratigraphic position, and the paleoenvironmental reconstruction of the last phase of the Amazon Basin settling. This study describes, for the first time, the occurrence of fossil wood in outcroppings of the left bank of the Amazon River, where anatomical and morphological data has enabled its characterization to the species level. Thus, the data marks the record of the Annonaceae in South America, as well as the depositional processes related to incorporation of organic material in the sandy layer and the fossilization processes that allowed its preservation. In an unprecedented way, this study has described Duguetiaxylon amazonicum nov. gen and sp. and provided information on the anatomical and systematic character, as well as data on plant-insect interaction, and a better understanding of the family.

On the formation and evolution of the Pannonian basin: constraints derived from the orogenic collapse recorded at the junction between Carpathians and Dinarides

Science.gov (United States)

Matenco, L. C.; Radivojevic, D.

2012-04-01

Formation and evolution of back-arc basins is related to the evolution of subduction zones, resulting geometries being dependent on the interplay between the velocity of retreating slabs and boundary conditions that often limit rapid subduction systems. Classical models of evolution in the Alps-Carpathians-Dinaridic domain assume that the formation of the Pannonian back-arc basin is related to the rapid roll-back of an European slab and the invasion of Tisza-Dacia and ALCAPA upper plate blocks into the so-called Carpathians embayment starting at ~20Ma. The general mechanism assumes a gradual evolution, an initial mechanical phase of extensional detachments being recognized near the transition between the Alps and the Pannonian basin was subsequently followed by upper crustal normal faulting and a thermal phase during the Middle-late Miocene times that affected the central part of the Pannonian basin. A key area of the entire system often neglected by kinematic studies is the connection between South Carpathians and Dinarides. Here, regional seismic lines traversing the entire Serbian part of the Pannonian basin were calibrated with well data in order to derive an evolutionary model. The deformation is dominantly expressed by the formation of extensional (half-)grabens that are the brittle expression of large-scale extensional detachments. In contrast with previous interpretation restricting the syn-rift phase to the Middle Miocene, the geometry of normal faults and the associated syn-kinematic sedimentation allows the definition of a continuous Early to Late Miocene extensional evolution that was followed by the formation of isolated uplifted areas during the subsequent Pliocene - Quaternary inversion. The orientation of these (half-)grabens changes gradually from W-E to NW-SE and then to N-S, suggesting that the present-day strike of faults is the effect of a clockwise rotational mechanism of South Carpathians and Apuseni Mountains in respect to Dinarides. The S

Qu’elle était verte ma vallée

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Hervé Nicolle

2014-07-01

Full Text Available Le présent texte présente certaines des conclusions d’une étude conduite dans le district de Deh Sabz au Nord de la capitale Afghane, à l’automne 2011. Alors qu’un vaste projet urbanistique doit voir le jour dans les prochaines décennies sur le territoire de Deh Sabz, autrefois « vallée verte » de Kaboul, les nomades en transit dans le district voient leur genre de vie traditionnel profondément remis en cause. Les changements radicaux survenus depuis quarante ans, les discours opportunistes des prédateurs politiques locaux, l’alternance des sécheresses et inondations, ou la réduction des terres de pâture contribuent à accélérer un phénomène de sédentarisation – doublé d’une marginalisation socio-économique accrue. Cette perte d’identité des nomades Kuchi, parce qu’elle ne s’accompagne d’aucune contrepartie, comporte un risque politique important à l’heure où le pays doit faire face à une transition politique aux contours incertains, ainsi qu’à une criminalité et une insécurité accrues.

La formación racial y resignificación de la justicia social en el Valle del Chota

OpenAIRE

Zambrano Murillo, María Giulianna

2010-01-01

El objetivo de este trabajo es analizar la movilización social afroecuatoriana desde lo local y, para ello, se concentrará en el estudio de las organizaciones sociales en el Valle del Chota a través de la historia. La reducción del alcance responde a la escasa bibliografía que documenta las dinámicas locales de las organizaciones, especialmente cuando pasan a formar parte de un movimiento nacional, y también a la necesidad de recuperar la historia y las necesidades específicas de las comunida...

La institucionalidad turística y el desarrollo de dos productos turísticos del valle del Colca

OpenAIRE

Aronés Ochoa, Cedy Calissa

2014-01-01

Universidad Nacional Agraria La Molina. Escuela de Posgrado. Maestría en Ecoturismo La presente tesis de maestría aborda el estudio de dos productos turísticos en el Valle del Colca (Caylloma, Arequipa – Perú), a partir de la observación de los fenómenos socio políticos suscitados entre el 2002 – 2012. Con el estudio se busca identificar las principales características de dos productos turísticos distintivos del destino Colca, analizar la construcción de la institucionalidad turística en e...

CÓMO LLEGAN A LA DEFINICIÓN DE LA ESTRATEGIA LAS EMPRESAS LOCALIZADAS EN EL VALLE DE ABURRÁ

OpenAIRE

Alejandro, Ramos

2008-01-01

Este artículo está enfocado a entender las variables y determinantes de las ideas sobre cómo llegan a la estrategia expresadas por personas que trabajan en empresas localizadas en el valle de Aburrá. El método empleado para realizar la investigación que soporta este artículo fue de carácter exploratorio con enfoque cualitativo, recolectando la información mediante un trabajo de campo por medio de una guía semiestructurada de preguntas abiertas, para posteriormente hacer el análisis y observac...

Determination of elements in the atmosphere of Valle de Toluca by Neutron Activation (July 1992 - April 1993)

International Nuclear Information System (INIS)

Garcia S, I.

1994-01-01

The purpose of this study is to continue with the environmental monitoring program of Valle de Toluca by means of the Neutron Activation Analysis and atomic absorption techniques. The analytical results corresponding to the period of July 1992 to April 1993, and the analyzed elements by Neutron Activation were Na, V, Br, Al and Mn, while Cr and Pb were analyzed by Atomic Absorption Spectroscopy. Since the study is a joint project with the Facultad de Quimica de la Universidad Autonoma del Estado de Mexico, the purpose is to continue with this type of chemical analysis. (Author)

Grafismo mueble en el Valle de Côa (Vila Nova de Foz Côa, Portugal: la estación arqueológica de Fariseu

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Marcos GARCÍA DIEZ

2013-05-01

Full Text Available El repertorio de arte mueble paleolítico en territorio portugués es muy reducido. Durante los trabajos arqueológicos realizados, con carácter de urgencia en diciembre de 1999, en la estación de Fariseu (Vila Nova de Foz Côa, Portugal se localizaron dos plaquetas de esquisto en contexto estratigráfico. A falta de dataciones radiométricas de los niveles arqueológicos, y sobre la base del estudio de las evidencias líticas, la primera de ellas, con un rico repertorio temático, se adscribe a momentos finales del Magdaleniense. La segunda, con sólo una figura zoomorfa, se relaciona con ocupaciones del Magdaleniense antiguo o Protosolutrense. Se realiza una valoración de las evidencias dentro del contexto peninsular, prestando especial atención a la vertiente mediterránea, y se relacionan con el grafismo rupestre del valle de Côa, aportando así elementos de inserción cronológica para caracterizar el amplio repertorio rupestre del valle de Côa.

Lista anotada y clave para las ranas (género Eleutherodactylus chocoanas del Valle del Cauca, y apuntes sobre las especies de la Cordillera Occidental adyacente

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Lynch John Douglas

1999-11-01

Full Text Available Twenty-three species of the genus Eleutherodactylus are reported fram 24 localities in the western lowlands of Valle del Cauca, Colombia, with notes on their identificacion and distributions. Up to 16 species have been taken from a single site. The cloud forest fauna of  Eleutherodactylus found on the Cordillera Occidental above the drainages of the Anchicayá, Cajambre, Calima, and Dagua rivers consists of 24 species with up to 18 species being found in a single site.Se da información sobre la identificación y las distribuciones de 23 especies del género Eleutherodactylus de 24 sitios de las tierras bajas del occidente del Valle del Cauca, Colombia. Hasta 16 especies fueron registradas del mismo sitio. La fauna de Eleutherodactylus de los bosques nublados de la Cordillera Occidental en los drenajes de los ríos Anchicayá, Cajambre, Calima, y Dagua consta de 24 especies, con hasta 18 encontradas en un mismo sitio.

Coleópteros acuáticos y semiacuáticos del Parque Provincial Salto Encantado y Valle del Cuñá Pirú (Misiones, Argentina Aquatic and semiaquatic Coleoptera from Salto Encantado y Valle del Cuñá Pirú Provincial Park (Misiones, Argentina

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Liliana A. Fernández

2008-12-01

Full Text Available Se presentan los resultados de la recolección de coleópteros acuáticos y semiacuáticos del Parque Provincial Salto Encantado y Valle del Cuñá Pirú, con el objeto de contribuir al conocimiento de la biodiversidad del área protegida mencionada, de la provincia de Misiones. Los sitios de muestreo incluyeron ambientes lóticos y lénticos. Se registraron 74 especies de coleópteros, distribuidas en 44 géneros y 14 familias: Haliplidae, Noteridae, Dytiscidae, Gyrinidae, Hydrochidae, Hydrophilidae, Hydraenidae, Staphylinidae, Scirtidae, Psephenidae, Limnichidae, Lutrochidae, Dryopidae y Elmidae. Se mencionan nuevas citas para la provincia y para la Argentina, así como la presencia de especies nuevas para la ciencia.This paper presents a list of aquatic and semiaquatic Coleoptera collected during a biodiversity study carried out in Salto Encantado and Valle del Cuñá Pirú Provincial Park. This study aims to improve the knowledge of this protected area located in Misiones Province. Permanent and semi-permanent lotic and lentic habitats were sampled. Seventy-four species of beetles in 44 genera and 14 families were recorded: Haliplidae, Noteridae, Dytiscidae, Gyrinidae, Hydrochidae, Hydrophilidae, Hydraenidae, Staphylinidae, Scirtidae, Psephenidae, Limnichidae, Lutrochidae, Dryopidae and Elmidae. New records for the province and for Argentina are listed, and the presence of new species is mentioned.

El cuaternario del Valle Inferior del Manzanares (Cuenca de Madrid, España

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Silva, P. G.

2003-08-01

the water and sediment supply during the end of cold periods with relevant neotectonic and karstic activity, feedback by significant intrabasinal headward erosion processes from the late Middle Pleistocene.Se analiza el tramo Inferior del Manzanares entre Villaverde y su desembocadura en el río Jarama. En este tramo, el valle es de carácter asimétrico con desarrollo de escarpes en Yesos (ea. 60 m en su margen izquierda y de terrazas complejas en su margen derecha. Dentro de ellas la que domina la geomorfología del sector es un nivel de terraza complejo (engrosado que denominamos TCMZ (+ 16-22 m. Se encuentra constituido por al menos cinco secuencias fluviales (Mz de tipo meandriforme. Sobre ellas se solapan a doble vertiente niveles mixtos (Mx desde los + 15 a los + 8 m que poseen un carácter (más braided. En la arquitectura de la TCMZ participan muy significativamente aportes laterales procedentes de los tributarios (Butarque y Culebro, de los relieves marginales (escarpes en yesos y de los propios sistemas de terrazas (derrames de escarpes. La TCMZ es el nivel más alto en este sector sobre el que, además, se instala la propia divisoria del Valle en este sector, constituyendo este hecho el carácter más anómalo del valle. Todos estos caracteres poco usuales son resultado directo de la respuesta del sistema fluvial al proceso de captura que sufrió por parte del Jarama durante el Pleistoceno medio. Los contenidos faunísticos y líticos de la TCMZ permiten situar su desarrollo entre los OIS 10 (? al 5. Una manifiesta crisis paleosísmica a comienzos del OIS 5 acompaña al primer episodio de disección importante en el valle después del proceso de Captura. Las faunas frías e industrias musterienses de los niveles Mx permiten ubicar su desarrollo entre el OIS 4 y 3. En cualquier caso hay que considerar que los episodios de cut & fill que han modelado el paisaje fluvial durante el Pleistoceno superior difícilmente responden a los cambios eustáticos que

Red comunitaria para la gestión ambiental en el Valle de Aburrá

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Toro Maria Isabel

2011-11-01

Full Text Available Cuando se hace referencia al cuidado y protección del ambiente, uno de los aspectos de tener en cuenta es la vulnerabilidad social, puesto que es más vulnerable una población sin ningún tipo de organización, sin cohesión ni gestión comunitaria, que una com unidad organizada para protegerse y cuidarse y donde la mayoría participa, toma decisiones y actúa para su desarrollo. Para realizar una coordinación entre las organizaciones sociales existentes que trabajan por la protección y preservación de las condiciones ambientales de su territorio, se hace necesario la unificación de los papeles y perfiles de sus integrantes, sus objetivos, estrategias, proyectos e intervenciones en la búsqueda del bien común. Por lo anterior, el Área Metropolitana del Valle de Aburrá con la Universidad EAFIT diseñó e implementó una Red Comunitaria para la Gestión Ambiental, como un sistema organizado, abierto y participativo que fomenta los principios de voluntad, mutualidad, solidaridad, diversidad, tolerancia, comunicación, respeto, sentido de pertenencia y trabajo en equipo. La Red Comunitaria de Comités Ambientales del valle de Aburrá busca entonces retomar los antecedentes existentes en el campo de la preparación y participación comunitaria para la prevención y atención de emergencias y desastres, como los son las experiencias de los municipios de Medellín y Bello. Esta red tiene como fundamento los lineam ientos necesarios para articular las acciones, estrategias y com petencias de sus integrantes y las de aquellas personas que representan a las autoridades ambientales, administraciones municipales y organismos de socorro, que son pilares de apoyo dentro de una estructura integral para un grupo especializado en la problemática ambiental y de gestión del riesgo.

The Evolution of Juventae Chasma, Valles Marineris, Mars: Progressive Collapse and Sedimentation

Science.gov (United States)

Fueten, F.; Novakovic, N.; Stesky, R.; Flahaut, J.; Hauber, E.; Rossi, A. P.

2017-11-01

Juventae Chasma is an isolated chasm located north of the interconnected chasms within Valles Marineris. It contains four separate interior layered deposit (ILD) mounds. We have combined layer measurements, as well as mineralogical data of the mounds with topographic data of the remaining chasm and the surrounding plateau. Our observations indicate that the chasm underwent a complex geological history. We suggest that individual ILD mounds are not contemporaneous with each other and a series of progressive collapses enlarged an initially smaller chasm to its current shape. ILDs were deposited in a lacustrine setting, and the time of ILD deposition was limited. Basin collapse and chasm enlargement continued beyond the time of ILD deposition and thus were not driven by sediment load. Glacial processes appear to have played a role in the late, postlacustrine history of the chasm. We present a simplified model that highlights some of the complexity of the chasm evolution, but acknowledge that the true history is undoubtedly more complicated.

Movilidad Espacial, Ocupación y Empleo en el Valle Inferior del Río Chubut Spatial mobility, Occupation and Employment in the Inferior Valley of the River Chubut

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M. Marcela Crovetto

2011-12-01

Full Text Available Desde una perspectiva que propone una serie de críticas a la tipología dicotómica de clasificación demográfica del espacio habitado, rural y urbano, se ha indagado sobre las formas que adquiere la movilidad espacial cotidiana en relación al empleo y a la ocupación en el Valle Inferior del Río Chubut -patagonia argentina-, atendiendo a una situación especial de movilidad espacial cotidiana como es la referida a la producción de cerezas en el Valle. Se utilizaron fuentes secundarias estadísticas, históricas y documentales en articulación con la construcción de datos primarios mediante relevamientos operados por distintas técnicas. Fundamentalmente se aplicó una encuesta a hogares (200 casos de barrios periféricos de las localidades involucradas en el Valle Inferior del Río Chubut El centro del ejercicio de la investigación estuvo en contraponer los resultados de una encuesta realizada en campo de acuerdo tanto a la clasificación clásica de la zona de residencia (rural o urbana como a una propuesta alternativa para la investigación. Así se evaluaron los matices escondidos dentro de las homogeneizantes ideas de rural y urbano, sintetizadas por la cantidad de habitantes -en Argentina con 2000 o más se considera un espacio urbano, con menos un espacio rural- observándose, especialmente, que muchas trayectorias cotidianas de actores sociales considerados clásicamente urbanos se acercaban mucho a las de los actores de las zonas rurales.From a perspective that proposes a number of criticisms of the dichotomous typology of demographic classification of living space, rural and urban, has inquired about the forms that everyday spatial mobility in relation to employment in the Valle Inferior del Río Chubut - Patagonia-Argentina, following a special situation of everyday spatial mobility as that concerning the production of cherries in the Valley. Were used statistics, historical and documentary in coordination with the construction

Factores psicosociales que promueven la resiliencia en los niños trabajadores del municipio de Roldanillo-Valle del Cauca

OpenAIRE

Victoria Aguilar, Mariela

2011-01-01

Tesis (Maestría en Desarrollo Infantil). Universidad de Manizales. Facultad de Ciencias Sociales y Humanas, 2011 El resultado de la investigación, da respuesta al interrogante ¿Cuáles son los factores psicosociales que promueven la resilencia en los niños trabajadores del municipio de Roldanillo-Valle del Cauca? Para obtener esta información se identificaron factores de riesgo y factores protectores presentes en los niños trabajadores que se dedican específicamente a labores comerciales. E...

Vacancy induced half-metallicity in half-Heusler semiconductors

KAUST Repository

Zhu, Zhiyong; Cheng, Yingchun; Schwingenschlö gl, Udo

2011-01-01

First-principles calculations are performed to investigate the effect of vacancies on the electronic structure and magnetic properties of the two prototypical half-Heusler semiconductors NiTiSn and CoTiSb. The spin degeneracy of the host materials

Correlación de variables macroclimáticas del Océano Pacífico con los caudales en los ríos interandinos del Valle del Cauca (Colombia

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Yesid Carvajal

2014-06-01

Full Text Available Los fenómenos climáticos sobre los océanos ejercen gran influencia sobre la hidroclimatología del valle del río Cauca (Colombia, en especial el evento "El Niño Oscilación Sur" (ENOS, que es responsable de la variabilidad climática en escalas de tiempo que van desde meses hasta décadas. Debido a esta dependencia, se estudió la correlación entre 8 variables indicadoras del clima en los Océanos Pacífico y Atlántico con los caudales medios mensuales de 8 ríos del valle del río Cauca. Las series cubren un período promedio de 40 años 1957-1997. Los resultados muestran las variaciones regionales de la situación hidrológica del valle del río Cauca respecto a las variables macroclimáticas. Los coeficientes de correlación indican que las variables que presentan mayor asociación con los caudales analizados son en su orden: Las temperaturas de la superficie del mar en las regiones Niño 3, Niño 3-4, Niño 4 Y SOl, mientras en el Atlántico, las mejores correlaciones las presentan: la Temperatura en el Trópico, en el Atlántico Norte (NATL y Atlántico Sur (SATL respectivamente.

Fracciones de fósforo en suelos del Valle del Cauca con diferentes sistemas de cultivo de café Phosphorus fractions in soils of the Valle del Cauca under different coffee crop systems

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Diana Milena Mejía Umaña

2011-07-01

Full Text Available El trabajo tuvo como objetivo evaluar la influencia de los sistemas de cultivo de café: orgánico, convencional y orgánico-mineral, sobre las fracciones de fósforo (P en suelos del departamento del Valle del Cauca, Colombia. Las mediciones por fraccionamiento secuencial reducido se hicieron en el Laboratorio de Suelos del Centro Internacional de Agricultura Tropical (CIAT. El análisis estadístico se ajustó a un modelo de diseño completamente aleatorio en un arreglo en parcelas divididas con tres tratamientos y tres repeticiones. Los resultados mostraron que los contenidos de las fracciones orgánicas de P disponible y P moderadamente disponible variaron (P This study was conducted in the department of Valle del Cauca (Colombia coffee growing zone to evaluate the response of planting coffee under different cropping systems: organic, conventional and organicmineral, on soil phosphorus fractions with volcanic influence. Sequential fractionation methodology adapted by the International Center of Tropical Agriculture was used. The statistical analysis consisted of a Complete Randomized Block Design under a split plot arrangement with three treatments and three replications. The results showed that contents of the organic fraction of available P and the moderately available P showed significant differences among the systems in which organic and conventional management was included, the conventional system had the lowest values. The organic-mineral system showed the highest contents of organic and inorganic phosphorus and the conventional system showed the lowest for these fractions of P. For the non available P fraction, it was found that organic systems had higher P content than the conventional system and, the organic-mineral system showed significant differences with respect to the rest. The total P showed a similar pattern to the fractions described. The low content in the conventional system can be explained by specific aspects of

Une approche écosanté pour le contrôle de la fièvre de la vallée du ...

International Development Research Centre (IDRC) Digital Library (Canada)

17 août 2016 ... La fièvre de la vallée du Rift est une maladie grave qui se transmet par la piqûre d'un moustique qui infecte l'être humain, le bétail et les animaux sauvages. De plus, les êtres humains peuvent contracter la maladie par tout contact avec des animaux infectés. La maladie s'est répandue dans toute l'Afrique ...

7 CFR 51.2295 - Half kernel.

Science.gov (United States)

2010-01-01

... 7 Agriculture 2 2010-01-01 2010-01-01 false Half kernel. 51.2295 Section 51.2295 Agriculture... Standards for Shelled English Walnuts (Juglans Regia) Definitions § 51.2295 Half kernel. Half kernel means the separated half of a kernel with not more than one-eighth broken off. ...

Geomorphologic, stratigraphic and sedimentologic evidences of ...

Indian Academy of Sciences (India)

The EPF particularly has acted significantly and influenced in evolving the geomorphological landscape and the stratigraphic architecture of the area. The block bounded by the two faults has earlier been considered as a single entity, constituting a half-graben. The present investigation (by morpho-stratigraphic and ...

MEVTV workshop on tectonic features on Mars

International Nuclear Information System (INIS)

Watters, T.R.; Golombek, M.P.

1989-01-01

The state of knowledge of tectonic features on Mars was determined and kinematic and mechanical models were assessed for their origin. Three sessions were held: wrinkle ridges and compressional structure; strike-slip faults; and extensional structures. Each session began with an overview of the features under discussion. In the case of wrinkle ridges and extensional structures, the overview was followed by keynote addresses by specialists working on similar structures on the Earth. The first session of the workshop focused on the controversy over the relative importance of folding, faulting, and intrusive volcanism in the origin of wrinkle ridges. The session ended with discussions of the origin of compressional flank structures associated with Martian volcanoes and the relationship between the volcanic complexes and the inferred regional stress field. The second day of the workshop began with the presentation and discussion of evidence for strike-slip faults on Mars at various scales. In the last session, the discussion of extensional structures ranged from the origin of grabens, tension cracks, and pit-crater chains to the origin of Valles Marineris canyons. Shear and tensile modes of brittle failure in the formation of extensional features and the role of these failure modes in the formation of pit-crater chains and the canyons of Valles Marineris were debated. The relationship of extensional features to other surface processes, such as carbonate dissolution (karst) were also discussed

Las temperaturas del territorio que se extiende desde el Cantábrico Oriental al Valle del Ebro durante el periodo internacional 1961-90

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Javier M. Pejenaute Goñi

2001-01-01

Full Text Available El presente articulo tiene por objeto el estudio de las temperaturas en el territorio comprendido entre el Cantábrico oriental y el Valle del Ebro, durante el periodo internacional 1961-90. Este territorio está ocupado por las comunidades del País Vasco, Navarra, La Rioja y Aragón. Se estudian las temperaturas medias, las máximas, las mínimas, el coeficiente de variación y las heladas. También se incluye en el análisis anual, el estudio de la amplitud térmica, los quintiles y la tendencia futura.The present article aims at studying the temperatures in an área that goes from the cantábrico oriental and Valle del Ebro, for the international period of time going from 1961- 90. Four autonomous cornmunities. País Vasco, Navarra, La Rioja and Aragón, are included in this territory. The object of study will be the average, máximum and mínimum temperatures, as well as the coefficient of variation and freezes. It will also be included in the annual analysis. the study of thermal amplitude, quintiles, and future trend.

Petroleum systems of the Malay Basin Province, Malaysia

Science.gov (United States)

Bishop, Michele G.

2002-01-01

The offshore Malay Basin province is a Tertiary oil and gas province composed of a complex of half grabens that were filled by lacustrine shales and continental clastics.These deposits were overlain by clastics of a large delta system that covered the basin.Delta progradation was interupted by transgressions of the South China Sea to the southeast, which finally flooded the basin to form the Gulf of Thailand.Oil and gas from the Oligocene to Miocene lacustrine shales and Miocene deltaic coals is trapped primarily in anticlines formed by inversion of the half grabens during the late Miocene.Hydrocarbon reserves that have been discovered amount to 12 billion barrels of oil equivalent.The U.S. Geological Survey assessment of the estimated quantities of conventional oil, gas and condensate that have the potential to be added to reserves by the year 2025 for this province is 6.3 billion barrels of oil equivalent (BBOE) (U. S. Geological Survey World Energy Assessment Team, 2000).

Tucano Sul Basin: petroleum habitat; Bacia de Tucano Sul - habitat do petroleo

Energy Technology Data Exchange (ETDEWEB)

Schaller, Hannfried; Magalhaes, Celso Carvalho; Carvalho, Renato Kramberger

2008-07-01

The South Tucano Basin is located in the State of Bahia, and is an integrating part of the Northeast Brazilian intracratonic graben system which embraces the Jatoba, Tucano (North, Central and South), and Reconcavo Basins. It comprises a Late Jurassic - Early Cretaceous system of half grabens that evolved during the preliminary stages of continental break related to the South Atlantic opening, from which it was aborted during the Aptian. Close to one hundred wells have so far been drilled in the area, leading to the discovery of about 35 million m{sup 3} (220 mmboe) of oil equivalent, comprised in about ten small oil and gas pools, among which Conceicao, Querera, Lagoa Branca, Estacao de Irai and Sempre Viva . Organic shales, that area found in the lower half of the Candeias Fm, are interpreted as the main source rocks, and in regard to the stratigraphic position of the oil pool, three petroleum-systems are recognized in the basin: Candeias-Sergi; Candeias-Candeias, and Candeias-Ilhas. (author)

Dynamic half-rate connections in GSM

NARCIS (Netherlands)

Winands, E.M.M.; Wieland, J.; Sanders, B.

2006-01-01

Dynamic half-rate is an optional feature that allows a Global System for Mobile communication (GSM) cell to switch new incoming half-rate capable calls to half-rate speech coding, when the cell is nearly congested. Since two half-rate speech calls can be put together in one single-time slot, dynamic

EL PATRIMONIO ARQUEOLÓGICO COMO RECURSO: POLÍTICAS ESTATALES DE GESTIÓN EN TUCUMÁN Y TAFÍ DEL VALLE / The archaeological heritage as a resource: State policies and management in Tucuman and Tafi del Valle

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Barbara Manasse

2010-12-01

Full Text Available El territorio tucumano, en el centro del Noroeste argentino, es un área conocida por la riqueza de sus manifestaciones culturales materiales. Desde los comienzos de la constitución del Estado, Tucumán fue locus de distintas políticas y propuestas que las implicaban. Es factible rastrearlas en el accionar concreto sobre esos recursos culturales, así como también en los proyectos que se fueron planteando. Abordaremos un primer análisis de cómo desde el Estado se fue dibujando, definiendo, en fin, construyendo el “patrimonio arqueológico” en la provincia de Tucumán, en tanto conjunto de bienes culturales materiales que representaría parte del pasado local y que, por ende, merecería recibir un trato especial a los fines de garantizar su resguardo y conservación. Nuestro eje de estudio se centra en la materialidad indígena prehispánica del del Valle de Tafí en el Oeste tucumano indagando los diversos procesos y tomando en cuenta los diferentes actores que fueron configurando su patrimonialización en los contextos históricos, políticos y sociales de los últimos cien años. Consideramos que es un caso que puede ser paradigmático en pocos años más, tanto en lo que respecta al uso de los recursos culturales prehispánicos así como al destino de los mismos.Palabras clave: patrimonio; políticas estatales; arqueología; materialidades indígenas; Tafí del Valle.AbstractThe Tucuman region, located in the heart of Northwestern Argentina, is an area known for its wealth of cultural materials. From the earliest days of the nation, Tucuman has been a place where a wide range of policies and proposals have been advanced in relation to how these materials should be managed. It is therefore possible to review the concrete developments that have taken place along these lines, as well as the specifics of other projects that have been proposed.Here we undertake an initial analysis of how the State has engaged in the planning, definition

Early-Middle Pleistocene benthic turnover and oxygen isotope stratigraphy from the Central Mediterranean (Valle di Manche, Crotone Basin, Italy): Data and trends

OpenAIRE

Michele Azzarone; Patrizia Ferretti; Veronica Rossi; Daniele Scarponi; Luca Capraro; Patrizia Macrì; John W. Huntley; Costanza Faranda

2018-01-01

Ostracod faunal turnover and oxygen isotope data (foraminifera) along the Valle di Manche (VdM) section are herein compiled. Specifically, the material reported in this work includes quantitative palaeoecological data and patterns of ostracod fauna framed within a high-resolution oxygen isotope stratigraphy (δ18O) from Uvigerina peregrina. In addition, the multivariate ostracod faunal stratigraphic trend (nMDS axis-1 sample score) is calibrated using bathymetric distributions of extant mollus...

Tectonostratigraphic history of the Neogene Maimará basin, Northwest Argentina

Science.gov (United States)

Galli, Claudia I.; Coira, Beatriz L.; Alonso, Ricardo N.; Iglesia Llanos, María P.; Prezzi, Claudia B.; Kay, Suzanne Mahlburg

2016-12-01

This paper presents the tectonostratigraphic evolution of the Maimará Basin and explores the relationship between the clastic sediments and pyroclastic deposits in the basin and the evolution of the adjacent orogeny and magmatic arc. The sedimentary facies in this part of the basin include, in ascending order, an ephemeral fluvial system, a deep braided fluvial system and a medial to distal ephemeral fluvial system. We interpret that Maimará Formation accumulated in a basin that has developed two stages of accumulation. Stage 1 extended from 7 to 6.4 Ma and included accelerated tectonic uplift in the source areas, and it corresponds to the ephemeral fluvial system deposits. Stage 2, which extended from 6.4 to 4.8 Ma, corresponds to a tectonically quiescent period and included the development of the deep braided fluvial system deposits. The contact between the Maimará and Tilcara formations is always characterized by a regional unconformity and, in the study area, also shows pronounced erosion. Rare earth element and other chemical characteristics of the tuff intervals in the Maimará Formation fall into two distinct groups suggesting the tuffs were erupted from two distinct late Miocene source regions. The first and most abundant group has characteristics that best match tuffs erupted from the Guacha, Pacana and Pastos Grandes calderas, which are located 200 and 230 km west of the study area at 22º-23º30‧S latitude. The members the second group are chemically most similar to the Merihuaca Ignimbrite from the Cerro Galán caldera 290 km south-southwest of the studied section. The distinctive geochemical characteristics are excellent tools to reconstruct the stratigraphic evolution of the Neogene Maimará basin from 6.4 to 4.8 Ma.

Morfología básica de 17 introducciones del género Ocimum en el departamento del Valle

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Estrada Edgar Iván

1987-09-01

Full Text Available Los objetivos del trabajo fueron establecer un jardín de introducciones de albahaca y contribuir en la caracterización botánica de las cultivariedades introducidas al banco de germoplasma. La colección se realizó en el departamento del Valle en campos de cultivo, áreas de vegetación natural, huertos caseros y mercados locales. En 6 zonas se recolectaron 17 introducciones, pertenecientes a 5 especies del genero Ocimum tres cultivadas (O. basilicum L., O. americanum Jacq Host y 0. minimum L. y dos ornamentales (O. gratissimum Hook y O. micranthum Willd. Se determinó visualmente alta variación para características fenotípicas tales como arquitectura de plantas, presencia de pubescencia, tipo de inflorescencia, flores, hojas y frutos.The objetives of this work were the collection and stablishment of a garden of albahaca and a contribution to the botanical characteristic of the cultivars introduced in the germoplasm bank .The collection was gathered at cultivated fields, natural vegetation areas, house gardens and local markets. Seventeen (17 species were collected, all belonging to the generous Ocimum from six different zones of Valle del Cauca. Three species are cultivated (O. basilium L., O. americanum Jack Host y O. minimum L. and two are considered ornamentals (O. gratissimum Hook y O. micranthum Willd. Phenotipicaly, high variety was observed in the plant architecture, in its pubescence presence, in the type of inflorescence and in flowers, leaves and fruits.

Application of the business model Canvas in Microenterprises from Partners of the Savings and Credit Cooperative Luz del Valle

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Francisco Javier Monroy Espinosa

2017-12-01

Full Text Available The "Luz del Valle" Savings and Credit Cooperative is a financial institution with five thousand microentrepreneurial partners who have business units. These business units, generally informal, do not have a defined organizational structure or adequate management tools, which influences in the presence of economic problems such as arrears and non-payment of contracted obligations, mainly as a result of a low level of sales. Due to this situation, it is important for cooperatives to support their partners in finding solutions. This is part of the cooperative principles and values of mutual aid, social responsibility and education, training and information for its members, team leaders, managers and employees; these universal principles established by the International Cooperative Alliance (ICA are considered by the savings and credit cooperative "Luz del Valle" as strategies to accompany its partners in the development and growth of their business units. The cooperative organizes a Christmas Fair annually, where 60 microentrepreneurs participate. This event was the opportunity to develop, together with the Metropolitan University of Ecuador, a project that, in its first phase, trained in the formulation of strategies based on the application of the Business Model Canvas; the teaching of this tool, which allows creating, capturing and providing value for clients, was supported by the university community and the program of linkage with society that develops the aforementioned institution; the evaluation of the impact and the economic results are contemplated in a second phase.

Construcción rural como representación. Infraestructura agrícola menor en el valle central de Chile

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Juan Paulo Alarcón

2017-11-01

Full Text Available Los gallineros, secadores de maíz, bodegas, caballerizas, etc. del valle central de Chile son construcciones menores que funcionan como infraestructuras que complementan la producción agrícola básica y de pequeña escala que allí se desarrolla con lo cual su resolución, que roza lo arcaico, está desprovista de un germen disciplinar. Estas construcciones, si bien pueden ser la culminación material de una idea, más bien se plantean como la representación en sí misma de un proyecto, en un estado pendiente de resolución, que se ha ido forjando generación tras generación. Esparcidas en el territorio, representan tanto el carácter agrícola de la zona, como la inteligencia desplegada a lo largo del tiempo, determinada por las condiciones geográficas, culturales y sociales, en un contexto de escasez. Si bien tiene antecedentes en las edificaciones residenciales primitivas, se origina como tipo en la reforma agraria, cuando se reparten las tierras en superficies pequeñas que promueven el desarrollo de la agricultura menor. Las construcciones rurales en el valle central de Chile son en sí mismo la representación de su proyecto y, como manifestaciones, representan una actividad comunal, un territorio, un paisaje, un modelo económico, un ideal político.

Indagini Stratigrafiche e Sistemi Informativi Architettonici: il GIS della chiesa di S. Maria in Valle Porclaneta

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Trizio, Ilaria

2009-12-01

Full Text Available The church of Santa Maria in Valle Porclaneta and its accessories are what remains of an ancient Benedictine monastery, built in the heart of Abruzzo region (Magliano dei Marsi, L’Aquila at the end of the XII century. Even if literature, starting from the end of XIX century, has been often interested in this architectural manufactured, the process of historical-critical knowledge of the complex revealed itself difficult due to the absence of archaeological data, the shortage of the documents and, above all, the numerous interventions of restoration that, followed during all last century, have deeply modified the original compages of it. Due to the difficulties met, the overlap between the few documental data and the data derived from the direct investigation of the structures, performed with the aid of an Architectural Informative System, made possible to hypothesize a chronological reconstruction of the principal phases of life of the monastic complex.[it] La chiesa di Santa Maria in Valle Porclaneta e i suoi ambienti accessori sono quanto resta di un antico monastero benedettino, edificato nel cuore del territorio abruzzese (Magliano dei Marsi, L’Aquila sul finire del XII secolo. Sebbene la letteratura, a partire dalla fine dell’Ottocento, si sia spesso occupata di questo manufatto, il processo di conoscenza storico-critica del complesso si è rivelato difficoltoso a causa dell’assenza di dati archeologici, della scarsità di fonti documentarie pervenute, e, soprattutto a causa del susseguirsi di numerosi interventi di restauro che, succedutisi senza soluzione di continuità per tutto il secolo scorso, ne hanno letteralmente stravolto la compagine originale. A fronte delle difficoltà incontrate, la sovrapposizione tra i pochi dati documentali e i dati derivati dall’indagine diretta delle strutture, eseguita con l’ausilio di un Sistema Informativo Architettonico ha consentito di ipotizzare una ricostruzione cronologica delle

Verruga y Uta en el valle de Huaillacayan (Dpto. de Ancash.: I. Determinación de los límites altitudinales de la zona endémica y de la incidencia de ambas enfermedades

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Arístides Herrer

1957-12-01

Full Text Available Se ofrece los resultados de observaciones epidemiológicas acerca de la enfermedad de Carrión (verruga peruana y la leishmaniasis tegumentaria (uta realizadas en el valle de Huaillacayán (10º18' de latitud Sur, tendientes a determinar los límites altitudinales de las respectivas zonas endémcias y la incidencia de ambas enfermedades en relación con la altura sobre el nivel del mar, obteniendo las siguientes conclusiones: 1. La zona endémica de la uta está comprendida entre los 900 y 3,000 metros de altura sobre el nivel del mar. También para la verruga el límite superior de la respectiva zona endémica está alrededor de los 3,000 metros. En este caso el límite inferior no ha sido determinado, debido a que la región comprendida entre el nivel del mar hasta los 780 metros de altura ha sido objeto de periódicas aplicaciones del insecticida DDT desde varios años atrás. No obstante, cabe suponer que en el valle de Huaillacayán la zona verrucógena descienda más que la utógena. 2. La incidencia tanto de la verruga como de la uta parece estar determinada fundamentalmente por la altura de las localidades sobre el nivel del mar. En la verruga la máxima incidencia se observa entre los 900 y 1,800 metros de altitud, y en la uta entre los 1,800 y 2,700 metros. 3. En el valle de Huaillacayán tanto la zona verrucógena como la utógena descienden más que en el valle del Rímac, que se encuentra a grado y medio de latitud al sur del de Huaillacayán.

Low permeability Neogene lithofacies in Northern Croatia as potential unconventional hydrocarbon reservoirs

Science.gov (United States)

Malvić, Tomislav; Sučić, Antonija; Cvetković, Marko; Resanović, Filip; Velić, Josipa

2014-06-01

We present two examples of describing low permeability Neogene clastic lithofacies to outline unconventional hydrocarbon lithofacies. Both examples were selected from the Drava Depression, the largest macrostructure of the Pannonian Basin System located in Croatia. The first example is the Beničanci Field, the largest Croatian hydrocarbon reservoir discovered in Badenian coarse-grained clastics that consists mostly of breccia. The definition of low permeability lithofacies is related to the margins of the existing reservoir, where the reservoir lithology changed into a transitional one, which is mainly depicted by the marlitic sandstones. However, calculation of the POS (probability of success of new hydrocarbons) shows critical geological categories where probabilities are lower than those in the viable reservoir with proven reserves. Potential new hydrocarbon volumes are located in the structural margins, along the oil-water contact, with a POS of 9.375%. These potential reserves in those areas can be classified as probable. A second example was the Cremušina Structure, where a hydrocarbon reservoir was not proven, but where the entire structure has been transferred onto regional migration pathways. The Lower Pontian lithology is described from well logs as fine-grained sandstones with large sections of silty or marly clastics. As a result, the average porosity is low for conventional reservoir classification (10.57%). However, it is still an interesting case for consideration as a potentially unconventional reservoir, such as the "tight" sandstones.

Del campo a la ciudad, el paisaje y la identidad en el Valle del Río Pardo, al norte de Minas Gerais, Brasil

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Fabiana Oliveira Araujo

2014-11-01

Con la llegada de la minería, un gran número de agricultores cambiará la incertidumbre del campo por un trabajo estable en las empresas mineras. En este trabajo se analizan las consecuencias en el paisaje cultural del Valle del Río Pardo, provocadas por esta transformación de la actividad económica de la población.

Uso racional y sostenible de los recursos hídricos del acuífero del valle de Toluca

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Jaime Gárfias Soliz

2008-01-01

Full Text Available El agua subterránea constituye la principal fuente de agua potable en el valle de Toluca, esto ha inducido a una sobreexplotación del acuífero, así como la extinción de zonas húmedas y una constante degradación de la calidad del agua, por lo cual es necesario adoptar medidas de protección, realizando una evaluación cuantitativa de la evolución del acuífero y sus efectos a partir de estudios detallados en un contexto multidisciplinario y de datos fiables. En un primer paso hacia esta meta, el presente artículo tiene como finalidad plantear estrategias de ordenación de este recurso en el marco de un sistema más integrado y equitativo que conlleve a una explotación adecuada y duradera del recurso hidráulico. En consecuencia, se examinan algunas de las opciones de políticas esenciales en relación con distintos aspectos de la gestión del agua, ya que brindan considerables posibilidades de ser catalizadoras de un proceso más amplio de reforma de las políticas y la gestión de los recursos hídricos. Finalmente se describen los pasos para evolucionar hacia el uso sostenible de las aguas subterráneas en el valle de Toluca, buscando una mejora del conocimiento base en el que se adaptan los enfoques administrativos de ecosistemas y la administración en el manejo de las aguas subterráneas.

Integrated interpretation of seismic and resistivity images across the «Val d'Agri» graben (Italy

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E. Ceragioli

2002-06-01

Full Text Available Val d'Agri is a «recent SSW - NNE graben» located in the middle of the Southern Apennines thrust belt «chain» and emplaced in Plio-Pleistocene.The recent sedimentation of the valley represents a local critical geophysical problem. Several strong near surface velocity anomalies and scattering degrades seismic data in different ways and compromises the seismic visibility. In 1998, ENI and Enterprise, with the contribution of the European Community (ESIT R & D project - Enhance Seismic In Thrust Belt; EU Thermie fund acquired two «experimental seismic and Resistivity lines» across the valley. The purpose of the project was to look for methods able to enhance seismic data quality and optimize the data processing flow for «thrust belt» areas. During the work, it was clear that some part of the seismic data processing flow could be used for the detailed geological interpretation of the near subsurface too. In fact, the integrated interpretation of the near surface tomography velocity/depth seismic section, built for enhancing the resolution of static corrections, with the HR resistivity profile, acquired for enhancing the seismic source coupling, allowed a quite detailed lithological interpretation of the main shallow velocity changes and the 2D reconstruction of the structural setting of the valley.

AGRICULTURA Y POTENCIAL PRODUCTIVO EN EL VALLE DE AMBATO, CATAMARCA, ARGENTINA (SIGLOS VI A XI D.C / Agriculture and productive potential in the Ambato Valley, Catamarca, Argentina (VI-XI centuries AD

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Germán Figueroa

2009-12-01

Full Text Available El control y acumulación de recursos económicos en el Valle de Ambato entre los siglos VI y XI d.C. ha sido considerado como un factor de suma importancia en el mantenimiento y reproducción de las diferencias sociales entre las personas. Se cree que el uso de sectores seleccionados del paisaje como áreas de producción agrícola se hallaba vinculado de manera funcional y organizacional con agregados residenciales o aldeas emplazadas en el fondo del valle. En dichos sectores, más precisamente sobre los faldeos de la sierra de la Graciana y del Ambato, se registró la presencia de infraestructura agrícola, tales como terrazas de cultivo, represas y canales. En este trabajo, se analizan los sistemas de cultivo y su potencial productivo en relación a los grupos humanos que habitaron el valle, para lo cual se lleva a cabo una caracterización del sistema hidro-agrícola y un análisis de su capacidad sustentadora en base a registros arqueológicos y observaciones etnográficas propias. Los resultados obtenidos permitirán discutir acerca de la posible existencia de un excedente económico, utilizado por un determinado sector de la población con el propósito de usufructuar los beneficios derivados del mismo.   Palabras clave: Valle de Ambato, Aguada, sistemas agrícolas, potencial productivo, excedente económico.   Abstract The control and accumulation of economic resources in the Ambato Valley between VI and XI centuries AD has been considered a key factor in the maintenance and reproduction of social differences between people. It is believed that the use of selected sectors of the landscape as agricultural production areas was functional and organizational associated with villages located in the valley bottom. In these sectors, and more precisely on the slopes of Graciana and Ambato mountain ranges, the presence of agricultural infrastructure was registered, such as farming terraces, dams and channels. In this paper, we analyze the

The Valle de Parras and phylloxera disaster, 1870-1910. Genesis and concolidation of a winery in times of crisis

OpenAIRE

Corona Páez, Sergio Antonio

2009-01-01

Durante la era independiente, uno de los principales rubros de la economía de la villa y ciudad de Parras, en México, fue la producción de vinos, aguardientes y licores. Durante el último tercio del siglo XIX, la demanda nacional de bebidas alcohólicas creció, aumentando así la importancia económica de Parras. Diversos cosecheros iniciaron procesos modernizadores, y entre ellos destacó la familia Madero. Pero al intentar diversificar las variedades de vitis vinífera, introdujeron al Valle de ...

Prevalencia de deserción escolar en embarazadas adolescentes de instituciones educativas oficiales del Valle del Cauca, Colombia, 2006

OpenAIRE

Mauricio Hernández; Iván Osorio

2011-01-01

Antecedentes: Partiendo de la institución educativa, se investigó la relación entre embarazo adolescente y deserciónescolar y como influía el grado escolar y la edad de la embarazada en su riesgo de deserción.Materiales y métodos: Se aplicó una encuesta voluntaria en 180 instituciones educativas oficiales del departamento delValle del Cauca, correspondiente a 112,470 estudiantes mujeres, encontrando 605 embarazadas. De estas, a 564 se les realizóuna entrevista por un profesional en psicología...

Prevalencia de deserción escolar en embarazadas adolescentes de instituciones educativas oficiales del Valle del Cauca, Colombia, 2006

OpenAIRE

Osorio, Iván; Hernández, Mauricio

2011-01-01

Antecedentes: Partiendo de la institución educativa, se investigó la relación entre embarazo adolescente y deserción escolar y como influía el grado escolar y la edad de la embarazada en su riesgo de deserción. Materiales y métodos: Se aplicó una encuesta voluntaria en 180 instituciones educativas oficiales del departamento del Valle del Cauca, correspondiente a 112,470 estudiantes mujeres, encontrando 605 embarazadas. De estas, a 564 se les realizó una entrevista por un profesional en psicol...

Patrimonio fotográfico del Valle del Cauca: el archivo de Otto Moll González

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Olga Cecilia Eusse González

2012-06-01

Full Text Available El Departamento Red de Bibliotecas, a través del Área Cultural de Cali, adquirió en 2009 el archivo fotográfico de Otto Moll González (Cúcuta, 1904-Cali, 1988. Este archivo, conformado por alrededor de 30.000 documentos entre negativos blanco y negro (en película y vidrio y fotografías blanco y negro en papel de diferentes formatos, constituye una de las colecciones de imágenes más valiosas que tiene el Valle del Cauca para los decenios de 1950 a 1980 y es un aporte importante a las colecciones documentales de la Red de Bibliotecas sobre el suroccidente y otras regiones del país.

Campground marketing: the heavy-half strategy

Science.gov (United States)

Wilbur F. LaPage

1969-01-01

When we arrayed camping frequencies in order from the lowest to the highest number of days spent camping per year we found that half of the campers do much more than half of the camping. Campers in this heavy half consistently camp more, year after year, and are increasing their annual participation as well. Heavy-half campers have larger investments in camping...

Une approche écosanté pour le contrôle de la fièvre de la vallée du ...

International Development Research Centre (IDRC) Digital Library (Canada)

17 août 2016 ... Ces conclusions sont particulièrement pertinentes à la lumière des avancées récentes réalisées pour le vaccin contre la fièvre de la vallée du Rift et seront un important facteur à prendre en compte pour le moment de lancer le futur vaccin et la manière de le faire. Les tendances de mobilité du bétail ...

Journal of Earth System Science | Indian Academy of Sciences

Indian Academy of Sciences (India)

... clastic input is attributed to the sedimentary response to basin tectonics. The sandstone–shale alternations of the Barren Measures succession can be correlated with the tectonic cyclothems developed on the hangingwall dip-slope and adjoining trough in a continental half-graben setting. Enhancement of the gradient of ...

Lesiones cutáneas por presión en adultos hospitalizados en el Hospital Universitario del Valle, Cali.

OpenAIRE

Gladys Eugenia Canaval; Natalia Tobo

2009-01-01

Durante un período de seis meses en adultos hospitalizados en el Servicio de Medicina Interna, Hospital Universitario del Valle (HUV), en Cali, Colombia, se identificó el riesgo de hacer lesiones cutáneas por presión, la presencia de las mismas y los factores que intervienen en su desarrollo . El riesgo de lesiones por presión se midió con la escala Braden entre las 36 y 48 horas del ingreso al servicio; se valoraron actividad física, movilidad, fricción, nutrición, percepción sensorial y hum...

Muestreo de suelos para la fertilización nitrogenada a tasa variable en el Valle del Cauca

OpenAIRE

Rojas Legarda, José Rafael

2015-01-01

En la actualidad el manejo de la fertilización para los lotes cultivados en caña de azúcar se hace como si fuera en grandes bloques uniformes a pesar de la gran variación que presentan los suelos en el Valle de Cauca, con el propósito de identificar la variabilidad del suelo y optimizar la distancia de toma de muestras se usaron datos provenientes de un muestreo sistemático en red de 20x20 metros en tres lotes para un área efectiva de 11.00 hectáreas y un total de 275 sitios. El suelo evalua...

Epidemiología de los nematodes gastrointestinales en caprinos lecheros en los valles templados del NOA, Argentina

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SUAREZ, V.H.

2013-08-01

Full Text Available Con el fin de estudiar la epidemiología y los efectos de los nematodes gastrointestinales (NGI sobre cabras en ordeño en predios bajo riego en el Valle de Lerma (Salta, se monitoreó la infestación parasitaria en 41 cabras naturalmente infestadas por NGI, desde el 4 de octubre de 2010 hasta el 26 de mayo de 2011. Se evaluaron dos grupos de cabras en ordeño: PJ (n=17 paridas en junio y PS (n=24 paridas en septiembre. Sólo se desparasitaron de urgencia aquellos animales que superaran los 3000 de hpg o y que presentaran signos de parasitosis.

Planar half-cell shaped precursor body

DEFF Research Database (Denmark)

2015-01-01

The invention relates to a half-cell shaped precursor body of either anode type or cathode type, the half-cell shaped precursor body being prepared to be free sintered to form a sintered or pre-sintered half-cell being adapted to be stacked in a solid oxide fuel cell stack. The obtained half......-cell has an improved planar shape, which remains planar also after a sintering process and during temperature fluctuations....

Empoderamiento y liderazgo femenino; su papel en la autogestión comunitaria en el corregimiento El Hormiguero - Valle del Cauca

OpenAIRE

María Isabel Erazo Caicedo; María del Carmen Jiménez Ruiz; Carmelina López Morales

2014-01-01

El presente artículo da a conocer el papel del empoderamiento de la mujer, y cómo este permite su rol esencial en lo económico, social y medioambiental, convirtiéndose así en un liderazgo transformacional que permite que sus voces sean escuchadas. Surge como producto del proyecto investigativo denominado Autogestión comunitaria para el desarrollo psicosocial del corregimiento El Hormiguero del municipio de Santiago de Cali (Valle del Cauca), elaborado por un grupo de profesores del programa d...

Trace metal distributions in the sediments from river-reservoir systems: case of the Congo River and Lake Ma Vallée, Kinshasa (Democratic Republic of Congo).

Science.gov (United States)

Mwanamoki, Paola M; Devarajan, Naresh; Niane, Birane; Ngelinkoto, Patience; Thevenon, Florian; Nlandu, José W; Mpiana, Pius T; Prabakar, Kandasamy; Mubedi, Josué I; Kabele, Christophe G; Wildi, Walter; Poté, John

2015-01-01

The contamination of drinking water resources by toxic metals is a major problem in many parts of the world, particularly in dense populated areas of developing countries that lack wastewater treatment facilities. The present study characterizes the recent evolution with time of some contaminants deposited in the Congo River and Lake Ma Vallée, both located in the vicinity of the large city of Kinshasa, capital of Democratic Republic of Congo (DRC). Physicochemical parameters including grain size distribution, organic matter and trace element concentrations were measured in sediment cores sampled from Congo River (n = 3) and Lake Ma Vallée (n = 2). The maximum concentration of trace elements in sediment profiles was found in the samples from the sites of Pool Malebo, with the values of 107.2, 111.7, 88.6, 39.3, 15.4, 6.1 and 4.7 mg kg(-1) for Cr, Ni, Zn, Cu, Pb, As and Hg, respectively. This site, which is characterized by intense human activities, is especially well known for the construction of numerous boats that are used for regular navigation on Congo River. Concerning Lake Ma Vallée, the concentration of all metals are generally low, with maximum values of 26.3, 53.6, 16.1, 15.3, 6.5 and 1.8 mg kg(-1) for Cr, Ni, Zn, Cu, Pb and As, respectively. However, the comparison of the metal profiles retrieved from the different sampled cores also reveals specific variations. The results of this study point out the sediment pollution by toxic metals in the Congo River Basin. This research presents useful tools for the evaluation of sediment contamination of river-reservoir systems.

Neogene biogenic sediments of onshore Peru. Part 2. Geochemistry and diagenesis

Energy Technology Data Exchange (ETDEWEB)

Baker, P.A.; Dunbar, R.B.; Marty, R.C.

1985-01-01

The Neogene sediments of coastal Peru are comprised in part of biogenic silica, phosphorites, and authigenic dolomites. The authors have studied these sediments in the Pisco Basin of southern Peru. In this region the sediments have escaped large-scale post-depositional structural or thermal overprinting. The phosphorites of the Middle Member of the Miocene Pisco Formation occur as 5 to 10 cm. thick beds of phosphatic sediments separated by meters of siliceous, tuffaceous, or dolomitic muds and silts. The phosphatic grains are usually colitic and the depositions are often channeled and reworked on a small scale. Many of these colitic beds disconformably overlie phosphatized dolomitic beds. The dolomites of the Pisco Formation occur as authigenic beds and nodules a few centimeters to over one meter in diameter. They occur at intervals of one to tens of meters. The dolomites are well-ordered and calcite-free. The mole percent calcium varies from 47.3 to 57.4, iron from 0.12 to 2.18, and manganese from 0.03 to 0.62. Strontium varies from 90 to 837 ppm, zinc from 12 to 124 ppm, and sulfate from 100 to 2000 ppm. The carbon isotopic composition of the Pisco dolomites is usually negative, varying from +7.05 to -21.86 per mil PDB. The oxygen isotopic compositions vary from -0.18 to +4.16 per mil PDB. These chemical signatures are consistent with rapid authigenic formation of the dolomite: (1) within a few meters of the sea floor, (2) at shallow water depths, (3) in sediments undergoing microbial sulfate reduction but in the presence of some dissolved sulfate, and (4) in the absence of thermal or fresh water diagenetic overprinting.

Más allá del valle del Rift: la evidencia arqueológica del Plio-Pleistoceno fuera de África Oriental

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Ignacio de la TORRE SÁINZ

2009-12-01

Full Text Available RESUMEN: La mayor parte de los trabajos sobre la arqueología del Plio-Pleistoceno en Africa se centran en la evidencia del valle del Rift. Allí existen extensas columnas crono-estratigráficas que permiten contextualizar de forma fiable los conjuntos arqueo-paleontológicos y reconstruir así la secuencia evolutiva de nuestro género. Se suele obviar de esa forma la evidencia del resto de África, donde existen grandes áreas sedimentarias muy poco conocidas desde un punto de vista arqueológico. En este trabajo se reflexionará sobre el registro arqueológico plio-pleistocénico en las zonas alejadas del valle del Rift, y se tratará de reconstruir cómo fue la primera colonización del continente africano.ABSTRACT: Most of the works about the African Plio-Pleistocene are focused on the Rift Valley evidence. In this area there are long chrono-stratigraphical columns that build reliable contexts for the archaeo-paleontological sites, providing the reconstruction of the evolutionary sequence of our Genus. Evidence on the rest of Africa, where there are poor-known sedimentary areas from an archaeological point of view, is usually dismissed. In this work we will reflect on the Plio-Pleistocene record beyond the Rift Valley, trying to reconstruct the first settlement of the African continent.

Methane leakage during the evolution of petroleum systems in the Western Canada Sedimentary Basin and the Central Graben area of the North Sea

Science.gov (United States)

Berbesi, L. A.; di Primio, R.; Anka, Z.; Horsfield, B.

2012-04-01

Around 500 to 600 Tg (1 Tg = 1012 g) of methane enter the atmosphere every year, mainly as product of microbial processes and combustion of fossil fuels and burning biomass. The importance of another source, the geologic emissions of methane, is up to now only loosely constrained. In this study, we addressed the potential methane emissions during the geological evolution of the Western Canada sedimentary basin (WCSB), which holds the largest oil sand accumulations in the world, and the Central Graben area of the North Sea. In the case of the WCSB, thermogenic gas generation and leakage at the sediment surface were addressed through 3D petroleum systems modeling. In this basin, the accumulated oil experienced intense biodegradation that resulted in large masses of biogenic methane. We quantified this latter mass though a two-step mass balance approach. Firstly, we estimated the rate of petroleum degradation and the magnitude of petroleum loss. After this, we calculated the mass of biogenic methane generated using a model that assumes hexadecane (C16H34) as representative of the saturated compounds (Zengler et al., 1999). Our 3D model suggests that 90000-150000 Tg of dry gas (mostly methane) could have leaked during the interval from 80 Ma to 60 Ma. Therefore, uniform leakage rates would have been in the order of 10-3-10-2 Tg yr-1. Biogenic methane generation could have taken place at rates of 10-4 to 10-2 Tg yr-1. However, the effective mass of thermogenic and biogenic methane reaching the atmosphere might have been up to 90% lower than calculated here due to methanotrophic consumption in soils (Etiope and Klusman, 2002). We addressed the thermogenic gas generation and leakage in the Central Graben through two different methods. The first is based on a previous 3D petroleum system modeling of the region (Neumann, 2006). The second consisted of calculating the mass of generated petroleum based on source rock extension and properties (Schmoker, 1994), and then

METODOLOGÍA PARA LA CARACTERIZACIÓN DE COMBUSTIBLES SÓLIDOS MADERABLES DEL ÁREA METROPOLITANA DEL VALLE DE ABURRÁ “AMVA”, COLOMBIA METHODOLOGY FOR THE CHARACTERIZATION OF SOLID WOODEN FUELS OF THE "VALLE DE ABURRÁ" METROPOLITAN AREA, COLOMBIA

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Erika Biviana Vásquez Sierra

2006-12-01

Full Text Available Este trabajo exhibe la forma de realizar protocolos para la toma de muestras y muestreo en laboratorios, con fines de análisis de propiedades físicas de la madera utilizadas en el sector industrial del Área Metropolitana del Valle de Aburrá y el beneficio que se logra al caracterizar y establecer las propiedades de las maderas más utilizadas. En esta investigación se presentan algunos de los parámetros más importantes para el muestreo, como la toma de muestras en pilas o arrumes de desperdicios, manejo de éstas en el laboratorio y otros que se hacen de gran importancia como es el punto de ignición. La metodología propuesta se basa en algunas de las normas internacionales ASTM del carbón, por la similitud que tiene con la madera y por la escasez de información en cuanto al muestreo de este tipo en maderas.This study illustrates the way to perform protocols, collect samples, and conduct laboratory analyses in order to characterize the physical properties of wood used in the industrial sector of the "Valle de Aburrá" metropolitan area and the gains obtained by characterizing the properties of the most frequently used woods. In this investigation some of the most important sampling parameters are presented, such as taking samples in piles or accumulations of waste, handling of these samples in the laboratory and others of great importance such as the ignition point. The proposed methodology is based upon some of the international ASTM coal norms, for the similarity it has with wood and for the lack of information on sampling this type in wood.

Half-time strategies to enhance second-half performance in team-sports players: a review and recommendations.

Science.gov (United States)

Russell, Mark; West, Daniel J; Harper, Liam D; Cook, Christian J; Kilduff, Liam P

2015-03-01

A number of intermittent team sports require that two consecutive periods of play (lasting for ~30-45 min) are separated by a 10-20 min half-time break. The half-time practices employed by team-sports players generally include returning to the changing rooms, temporarily relaxing from the cognitive and physical demands of the first half, rehydration and re-fuelling strategies, addressing injury or equipment concerns, and receiving tactical instruction and coach feedback. However, the typically passive nature of these actions has been associated with physiological changes that impair performance during the second half. Both physical and cognitive performances have been found to decline in the initial stages of subsequent exercise that follows half-time. An increased risk of injury has also been observed during this period. Therefore, half-time provides sports scientists and strength and conditioning coaches with an opportunity to optimise second-half performance. An overview of strategies thought to benefit team-sports athletes is presented; specifically, the efficacy of heat maintenance strategies (including passive and active methods), post-activation potentiation, hormonal priming, and modified hydro-nutritional practices are discussed. A theoretical model of applying these strategies in a manner that compliments current practice is also offered.

Synchronous Half-Wave Rectifier

Science.gov (United States)

Rippel, Wally E.

1989-01-01

Synchronous rectifying circuit behaves like diode having unusually low voltage drop during forward-voltage half cycles. Circuit particularly useful in power supplies with potentials of 5 Vdc or less, where normal forward-voltage drops in ordinary diodes unacceptably large. Fabricated as monolithic assembly or as hybrid. Synchronous half-wave rectifier includes active circuits to attain low forward voltage drop and high rectification efficiency.

Late Neogene deformation of the Chocolate Mountains Anticlinorium: Implications for deposition of the Bouse Formation and early evolution of the Lower Colorado River

Science.gov (United States)

Beard, Sue; Haxel, Gordon B.; Dorsey, Rebecca J.; McDougall, Kristin A.; Jacobsen, Carl E.

2016-01-01

Deformation related to late Neogene dextral shear can explain a shift from an estuarine to lacustrine depositional environment in the southern Bouse Formation north of Yuma, Arizona. We infer that late Neogene deformation in the Chocolate Mountain Anticlinorium (CMA) created a barrier that blocked an estuary inlet, and that pre-existing and possibly active structures subsequently controlled the local course of the lower Colorado River. Structural patterns summarized below suggest that the CMA absorbed transpressional strain caused by left-stepping segments of dextral faults of the San Andreas fault system and/or the eastern California shear zone and Gulf of California shear zone. For this hypothesis to be correct, about 200-250 m of post-6 Ma, pre- ~5.3 Ma uplift along the CMA crest would be required to cut off a marine inlet. The 220-km-long CMA, cored by the early Paleogene Orocopia Schist subduction complex, extends from the Orocopia Mountains (Calif.) southeastward through the Chocolate Mountains (parallel to the southern San Andreas fault). Where Highway 78 crosses the Chocolate Mountains (Fig. 1), the CMA turns eastward through the Black Mountain-Picacho area (Calif.) and Trigo Mountains (Ariz.) into southwest Arizona. It separates southernmost Bouse Formation outcrops of the Blythe basin from subsurface Bouse outcrops to the south in the Yuma area. South of Blythe basin the CMA is transected by the lower Colorado River along a circuitous path. Here we focus on the geology of an area between the central Chocolate Mountains and the Yuma Proving Grounds in Arizona. Specific landmarks include the southeast Chocolate Mountains, Midway Mountains, Peter Kane Mountain, Black Mountain, Picacho Peak, and Gavilan Hills. For simplicity, we refer to this as the eastern Chocolate Mountains.

"Hospital Universitàri Vall d'Hebron" edificio de 50 años de antigüedad ¿puede ser sostenible?

OpenAIRE

Soler López, Esther

2012-01-01

El objeto del proyecto es valorar, definir y proponer, el compromiso y la trayectoria sobre sostenibilidad medioambiental que tiene el “Hospital Universitari Vall d’Hebron” de Barcelona. Como herramienta de valoración se ha utilizado la certificación BREEAM ES Salud, por considerarse un elemento lo suficientemente extenso y comprometido en el tema se sostenibilidad de un edificio hospitalario en uso. BREEAM ES Salud, estudia diez categorías a las que otorga una puntuación se...

Local ecological knowledge related with marine ecosystems in two coastal communities: El Valle and Sapzurro

International Nuclear Information System (INIS)

Correa, Sandra Liliana; Turbay, Sandra; Velez, Madelene

2012-01-01

The inhabitants of the Colombian coastal populations of El Valle, in the Pacific, and Sapzurro, in the Caribbean Darien, have ecological knowledge about coastal ecosystems that is a result of their constant relation with the sea, through fishing and navigation. The sea is a source of food and economical resources, but it is also the sphere where the male personality is forged. The accurate knowledge about mangrove, coral, coral reef, beaches and fishing grounds has been enriched through the dialog between local inhabitants and researchers in the conservation biology field. However, the tensions with researchers and environmental authorities still exist. The paper suggests that local ecological knowledge studies could be a starting point for maintaining a more horizontal dialogue between environmentalist and the populations with livelihoods derived of fishing.

Arsenic Content of the Drinking Water Source, for the Guadiana Valley, Mexico; Contenido de arsenico en el agua potable de Valle del Guadiana, Mexico

Energy Technology Data Exchange (ETDEWEB)

Alarcon Herrera, Maria Teresa [Centro de Investigacion en Materiales Avanzados (Mexico); Flores Montenegro, Isela [Sistema Desentralizado de agua Potable y alcantarillado Durango (Mexico); Romero Navar, Pedro [Comision Nacional del Agua (Mexico); Martin Dominguez, Ignacio [Centro de Investigacion en Materiales Avanzados (Mexico); Trejo Vazquez, Rodolfo [Instituto Tecnologico de Aguascalientes (Mexico)

2001-12-01

In recent years, high levels of arsenic concentration have been detected in some drinking water sources of the Guadiana Valley (Durango and surrounding towns) in Mexico. These levels are above the limits recommended bye the world Health Organization (WHO) and the maximum levels allowed by the Mexican standards. due to the well.known toxicity of this element, this study set as its objective to determine in quantitative terms the arsenic content of the drinking water sources for the Guadiana Valley, as the first step in the way to solve environment problems, It was found that 59% of the sources in the south, northeast and Northwest zones of Durango exceed in 40% the maximum level established by Mexican standards for arsenic content. In the Guadiana towns, 48% of the sources surpass such levels even in 46%. If the maximum levels suggested bye the WHO are taken as the reference, then virtually all sources exceed such level. [Spanish] En los ultimos anos, en la region del valle de Gadiana (ciudad de Durango y poblados cercanos) se han detectado niveles de concentracion de arsenico (As) en algunos pozos de abastecimiento de agua potable que superan los limites recomendados por la Organizacion Mundial de la Salud(OMS) y el limite maximo permisible establecido por la legislacion mexicana. Dada la conocida toxicidad de dicho elemento, en el presente estudio se propuso determinar cuantitativamente el contenido de arsenico en los pozos de abastecimiento de agua potable del valle del Guadiana, como un primer paso hacia la solucion de la problematica ambiental. Se encontro que en la zona sureste, noroeste y noreste de la ciudad, en 59% de los pozos se excede hasta en 40% la concentracion de arsenico establecida como limite maximo por la legislacion mexicana. En las poblaciones del valle del Guadiana, 48% de los pozos superan los limites mencionados hasta en un 136%. Si se toma como referencia el limite maximo establecido por la OMS, practicamente todos los pozos exceden el

Delineating shallow Neogene deformation structures in northeastern Pará State using Ground Penetrating Radar

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Dilce F. Rossetti

2003-06-01

Full Text Available The geological characterization of shallow subsurface Neogene deposits in northeastern Pará State using Ground Penetrating Radar (GPR revealed normal and reverse faults, as well as folds, not yet well documented by field studies. The faults are identified mostly by steeply-dipping reflections that sharply cut the nearby reflections causing bed offsets, drags and rollovers. The folds are recognized by reflections that are highly undulating, configuring broad concave and convex-up features that are up to 50 m wide and 80 to 90 ns deep. These deformation structures are mostly developed within deposits of Miocene age, though some of the faults might continue into younger deposits as well. Although the studied GPR sections show several diffractions caused by trees, differential degrees of moisture, and underground artifacts, the structures recorded here can not be explained by any of these ''noises''. The detailed analysis of the GPR sections reveals that they are attributed to bed distortion caused by brittle deformation and folding. The record of faults and folds are not widespread in the Neogene deposits of the Bragantina area. These GPR data are in agreement with structural models, which have proposed a complex evolution including strike-slip motion for this area from the Miocene to present.A caracterização geológica de depósitos neógenos ocorrentes em sub-superfície rasa no nordeste do Estado do Pará, usando Radar de Penetração no Solo (GPR, revelou a presença de falhas normais e reversas, bem como dobras, ainda não documentadas em estudos de campo prévios. As falhas são identificadas por reflexões inclinadas que cortam bruscamente reflexões vizinhas, causando freqüentes deslocamentos de camadas. As dobras são reconhecidas por reflexões fortemente ondulantes, configurando feições côncavas e convexas que medem até 50 m de amplitude e 80 a 90 m de profundidade. Estas estruturas deformacionais desenvolvem-se, principalmente

Analysis of meteorological drought for Dagua river basin, Valle del Cauca, Colombia

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Nathalia González López

2016-06-01

Full Text Available Context: Extreme climatic events causes great challenges for social, economic and environmental sustainability of a region. Droughts affect agricultural activities significantly thus endangering the livelihoods and food security of rural populations, this is especially crucial for developing countries. The objective of this study is to characterize meteorological drought in Dagua river basin, Valle del Cauca. Method:  Intensity, magnitude, duration and frequency of drought events was estimated using the Standardized Precipitation Index (SPI, for semi-annual and annual groupings with records of 19 stations, during the period 1982-2011 Results: At least one drought was identified in each series; the area near to the subxerofític Basin region, exhibits more frequency of extremely strong drought and lower threshold of minimum precipitation; the largest percentage of spatial coverage of drought coincides with El Niño phenomena events, such as those that occurred in 91-92 to 09-10. Conclusions: The results obtained provide an approach for prediction and characterization of drought, and offer inputs to generate strategies for planning and mitigation of their impacts.

Late Paleogene-early Neogene dinoflagellate cyst biostratigraphy of the eastern Equatorial Atlantic

Science.gov (United States)

Awad, Walaa K.; Oboh-Ikuenobe, Francisca E.

2018-04-01

Six dinoflagellate cyst biozones (zone 1-zone 5, subzones 1a and 1b) are recognized in the late Paleogene-early Neogene interval of the Ocean Drilling Program (ODP) Site 959 (Hole 959 A), Côte d'Ivoire-Ghana Transform Margin in the eastern Equatorial Atlantic. The biozones are based on palynological analysis of 30 samples covering a 273.2-m interval with generally fair preservation and good to poor recovery. We propose a new age of Late Eocene (Priabonian) for subunit IIB as opposed to the previously published mid-Early Oligocene age (middle Rupelian). This age assignment is mainly based on the presence of Late Eocene marker taxa, such as Hemiplacophora semilunifera and Schematophora speciosa in the lower part of the studied interval. We also document for the first time a hiatus event within dinoflagellate cyst zone 3, based on the last occurrences of several taxa. This interval is assigned to an Early Miocene age and is barren of other microfossils. Furthermore, we propose new last occurrences for two species. The last occurrence of Cerebrocysta bartonensis is observed in the late Aquitanian-early Burdigalian in this study vs. Priabonian-early Rupelian in mid and high latitude regions. Also, the last occurrence of Chiropteridium galea extends to the latest Early Miocene (Burdigalian) in ODP Hole 959 A; this event was previously identified in other studies as Chattian in equatorial regions, and Aquitanian in the Northern Hemisphere mid-latitudes. We suspect that these differences are due to physical (offshore vs. nearshore) and latitudinal locations of the areas studied.

Microfracture pattern compared to core-scale fractures in the borehole of Soultz-sous-Forets granite, Rhine graben, France

Energy Technology Data Exchange (ETDEWEB)

Dezayes, C.; Villemin, T. [Universite de Savoie (France). Laboratoire de Geodynamique des Chaines Alpines, UPRES-A CNRS 5025; Pecher, A. [Universite Joseph Fourier, Grenoble (France). Laboratoire de Geodynamique des Chaines Alpines, UPRES-A CNRS 5025

2000-07-01

Microfractures appearing in thin section as fluid inclusion trails in quartz crystals were studied in four core samples of Soultz-sous-Forets granite. Their orientations in four series of three mutually perpendicular thin sections were estimated using a previously described apparent dip method and a new method involving measurements of strike and apparent dips. Three samples display three microfracture sets and one sample displays two sets. In all samples, one set is nearly vertical and strikes N-S. In two samples, one and two sets are nearly vertical and strike E-W. In two samples, two sets strike NW-SE: one is vertical, the other dips gently to the NE (or SW). Comparing microfracture and mesofractures sets in the same cores shows that (1) the N-S microfacture set is always dominant at both scales and (2) all other microfracture sets have no mesoscopic counterpart. The N-S microfracture sets could have been created during E-W extension of earliest Cenozoic age (Rhine Graben rifting). Differences between the two scales are explained by a {sigma}{sub 1}/{sigma}{sub 2} switching which occurred at the crystal scale and generated mutually perpendicular cracks.

Half-life measurement of 89Rb

International Nuclear Information System (INIS)

Guo Xiaoqing; Yuan Daqing; Xu Lijun; Chen Kesheng; Wu Yongle; Zheng Yanming; Yao Shunhe

2013-01-01

89 Rb is an important fission product used for monitoring possible release of fission products from fuel element. The half-life is one of important nuclear parameters. The half-life of 89 Rb was determined using reference source method with two sets of HPGe detectors by place-relay way. In reference source method, the ratio of net full- energy peak areas from the measure nuclide and the reference source was used to avoid the count correction caused by dead time and pileup. For the very short half-life of 89 Rb, the half-life iterative method was used in data analysis and the translation method was used in data unification. Finally, the measured half-life of 89 Rb is (14.41±0.04) min. (authors)

Productividad y adaptación del frijol ejotero en el Valle de México

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G. Esquivel-Esquivel

2006-01-01

Full Text Available Los ejotes son hortalizas de alta calidad nutritiva y en México existe tendencia a incrementar el consumo de esta leguminosa, por lo cual, el objetivo de este trabajo fue identificar variedades de frijol ejotero de diferente hábito de crecimiento, adaptadas al Valle de México con base en la productividad y calidad del ejote en dos fechas de siembra. Se estableció un experimento con 36 variedades de frijol (31 fueron de hábito de crecimiento determinado y 5 de hábito indeterminado, el 21 de mayo y 15 de junio de 2001, en Texcoco, Estado de México. Se registraron los días a floración, días a inicio de corte, días a madurez fisiológica, peso fresco, producción total y longitud de los ejotes, así como el rendimiento de semilla. En la primera fecha de siembra (PFS se evaluó el contenido de proteína y de fibra cruda en los ejotes. Se encontraron diferencias significativas (P≤0.01 para todas las variables cuantificadas. El descenso de la temperatura, el fotoperiodo y la disponibilidad hídrica redujo el número de cortes de ejote, de ocho en la PFS a cinco en la segunda. Las variedades de hábito indeterminado registraron, en promedio, mayor rendimiento total de ejotes y semilla. Ejotero 50, OR 900 y US No. 3 mostraron el mayor rendimiento de ejotes en la PFS y pueden usarse en siembras tempranas. US No. 3, E10-1, F2 y E10-2 sobresalieron en la segunda fecha y pueden utilizarse en siembras tardías. En las dos fechas de siembra, Bayo Alteño mostró resistencia a enfermedades y rendimiento de ejotes y de semilla alto, por lo que puede sembrarse para doble propósito (ejote y grano y como progenitor en el mejoramiento genético del frijol ejotero. El rendimiento y calidad obtenidos mostraron que es factible producir ejotes en el Valle de México

Construcción rural como representación. Infraestructura agrícola menor en el valle central de Chile

OpenAIRE

Juan Paulo Alarcón

2017-01-01

Los gallineros, secadores de maíz, bodegas, caballerizas, etc. del valle central de Chile son construcciones menores que funcionan como infraestructuras que complementan la producción agrícola básica y de pequeña escala que allí se desarrolla con lo cual su resolución, que roza lo arcaico, está desprovista de un germen disciplinar. Estas construcciones, si bien pueden ser la culminación material de una idea, más bien se plantean como la representación en sí misma de un proyecto, en un es...

Facies pattern of the middle Permian Barren Measures Formation ...

Indian Academy of Sciences (India)

dip-slope and adjoining trough in a continental half-graben setting. ... of the hangingwall dip-slope during reactivation of the basin margin faults ...... The thick accumulation of carbonaceous shale .... tion of cyclothems along the toe-zone of the fault ..... Petrol. 60 1–17. Talbot M R and Kelts K 1990 Paleolimnological signa-.

7 CFR 51.1441 - Half-kernel.

Science.gov (United States)

2010-01-01

... 7 Agriculture 2 2010-01-01 2010-01-01 false Half-kernel. 51.1441 Section 51.1441 Agriculture... Standards for Grades of Shelled Pecans Definitions § 51.1441 Half-kernel. Half-kernel means one of the separated halves of an entire pecan kernel with not more than one-eighth of its original volume missing...

PREFACE: Half Metallic Ferromagnets

Science.gov (United States)

Dowben, Peter

2007-08-01

Since its introduction by de Groot and colleagues in the early 1980s [1], the concept of half metallic ferromagnetism has attracted great interest. Idealized, half-metals have only one spin channel for conduction: the spin-polarized band structure exhibits metallic behavior for one spin channel, while the other spin band structure exhibits a gap at the Fermi level. Due to the gap for one spin direction, the density of states at the Fermi level has, theoretically, 100 & spin polarization. This gap in the density of states in one spin at the Fermi level, for example ↓ so N↓ (EF) = 0, also causes the resistance of that channel to go to infinity. At zero or low temperatures, the nonquasiparticle density of states (electron correlation effects), magnons and spin disorder reduce the polarization from the idealized 100 & polarization. At higher temperatures magnon-phonon coupling and irreversible compositional changes affect polarization further. Strategies for assessing and reducing the effects of finite temperatures on the polarization are now gaining attention. The controversies surrounding the polarization stability of half metallic ferromagnets are not, however, limited to the consideration of finite temperature effects alone. While many novel half metallic materials have been predicted, materials fabrication can be challenging. Defects, surface and interface segregation, and structural stability can lead to profound decreases in polarization, but can also suppress long period magnons. There is a 'delicate balance of energies required to obtain half metallic behaviour: to avoid spin flip scattering, tiny adjustments in atomic positions might occur so that a gap opens up in the other spin channel' [2]. When considering 'spintronics' devices, a common alibi for the study of half metallic systems, surfaces and interfaces become important. Free enthalpy differences between the surface and the bulk will lead to spin minority surface and interface states, as well as

Post-Neogene tectonism along the Aravalli Range, Rajasthan, India

Science.gov (United States)

Sen, Deepawati; Sen, Saurindranath

1983-03-01

The Aravalli Range runs southwest from Delhi for a distance of about 700 km. Its western margin is well defined, but the eastern margin is diffuse. Five geomorphic provinces are recognized in the study area: the western piedmont plains; the ridge and valley province which in the Central Aravallis occurs at two different heights separated by a fault scarp; the plateau province demarcated from the former by a fault scarp, confined to the Southern Aravallis, and occurring for a short stretch at two heights across another fault scarp; the BGC rolling plains east of the Range; and the BGC uplands south of the above. The scarps coincide with Precambrian faults. A series of rapids and water-falls, together with deeply entrenched river courses across the scarps and the youthful aspects of the escarpments with no projecting spurs, or straight river courses along their feet, all point unmistakably to a recent or post-Neogene vertical uplift along pre-existing faults. Presence of knickpoints at a constant distance from the Range in all west-flowing rivers, the ubiquitous terraces, and river courses entrenched within their own flood-plain deposits of thick gritty to conglomeratic sand, are indicative of a constant disturbance with a gradual rise of the Range east of the knickpoint, wherefrom the coarse materials were carried by the fast west-flowing streams. There is a differential uplift across the plateau scarp together with a right-lateral offset. This epeirogenic tectonism is ascribed to the collision of the Eurasian and the subducting Indian plates and to a locking of their continental crusts. By early Pleistocene, with the MBT gradually dying off, continued plate movement caused a flexural bending of the plate by a moment generated at the back, and a possible delinking of the continental crust along the zone of subduction. The felexural bending ripped open the Precambrian regional faults. The differential uplift and the difference in the distances of the nodes on two

La micro, pequeña y mediana empresa (MiPyME exportadora del sector textil confección en el Valle de Aburrá: hallazgos a partir de análisis de casos La micro, pequeña y mediana empresa (MiPyME exportadora del sector textil confección en el Valle de Aburrá: hallazgos a partir de análisis de casos

Directory of Open Access Journals (Sweden)

Marleny Cardona A.

2007-04-01

Full Text Available This article makes an approach to the small and médium sized enterprises (SME’s of the textile and apparel sector, taking into account the policies and institutions that supports them, as well as their international experience. The methodology used was case studies, for which a questionnaire was applied to 23 companies of the Valle de Aburra; the lack of knowledge and articulation of the businessmen appeared as the main element..Este trabajo realiza una aproximación a las empresas micro, pequeñas y medianas -MiPyMEs- del sector textil-confección, teniendo en cuenta las políticas e instituciones de apoyo y su experiencia internacional. La metodología empleada fue el análisis de casos, aplicando un cuestionario a 23 empresas del Valle de Aburra; el desconocimiento y la desarticulación de los empresarios sobresalió como principal respuesta en la aplicación de los cuestionarios.