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Sample records for alfonso basin gulf

  1. Production, exportation and preservation of silicoflagellates in Alfonso Basin, Gulf of California

    Science.gov (United States)

    Martínez-López, Aída; Álvarez-Gómez, Irela G.; Pérez-Cruz, Ligia; Verdugo-Díaz, Gerardo; Villegas-Aguilera, María Magdalena

    2016-03-01

    Limited areas of sea floor have the physiochemical conditions that allow for the formation and preservation of high resolution (yearly or close to yearly) laminated sediments that can function as a historic proxy for past oceanographic and climate conditions. We evaluated and established the fidelity of the sedimentary record in recording these signals by analyzing silicoflagellates production, changes in species composition, skeletal settling and their subsequent burial in bottom sediments at Alfonso Basin. The data series from December 2005 to February 2008 showed similar tendencies in both the vertical flux and overlying euphotic zone (Zeu) production of silicoflagellates. Both series were numerically dominated by Octactis pulchra with maxima values being recorded for the mixed water column period. Observed differences occurred during the studied years in both magnitude and in flux composition. The presence of a mixed assemblage with (warm-temperate-cold) species such as Dictyocha fibula var. robusta, Dictyocha epiodon and Distephanus speculum could be explained by a synchronization of trends between a predominantly positive Pacific Decadal Oscillation and a positive North Pacific Gyre Oscillation climate phases that were the background conditions underlying the early 2006 through 2007 El Niño event. A Morisita's similarity index value of 97.5% between winter trap and Zeu samples combined with an annualized settling factor of 0.45, suggests that Alfonso Basin is a favorable settling environment for silicoflagellates. However, core-top sediments showed an attenuation of record fidelity (burial factor = 0.25) resulting in a modified record for the production and settling of skeletons. O. pulchra that were not preserved in sediments as the dominant species and with this removal, the signal was also lost of the highest silicoflagellate production season (Mixing-cyclonic eddy periods) from the sedimentary record of the Alfonso Basin.

  2. Magnetic mineral study of Holocene marine sediments from the Alfonso Basin, Gulf of California - implications for depositional environment and sediment sources

    Directory of Open Access Journals (Sweden)

    L. Pérez Cruz

    2009-07-01

    Full Text Available Results of a rock magnetic study of marine sediments from the Alfonso Basin, Bay of La Paz are used to investigate sediment sources and depositional environment in the southern Gulf of California during the Holocene. Radiocarbon dating provides stratigraphic control, with age for the core bottom sediments of 7597-7831 cal. yr B.P. Magnetic signal is dominated by fine-grained titanomagnetites, derived from the silicic volcanic units surrounding the Bay of La Paz. Magnetic mineralogy is relatively homogenous as seen in bulk magnetic properties of low-field susceptibility, remanent intensity and coercivity. Magnetic hysteresis loops show strong variable paramagnetic components; after paramagnetic correction loops show saturation at low fields and high saturation magnetization values. Plots of hysteresis parameter ratios for domain state show that samples group in the pseudo-single domain field, with mixtures of single and multi-domain particles. Magnetic susceptibility log shows relatively high frequency dependence factors, particularly for the Middle Holocene, suggesting contribution of fine-grained superparamagnetic minerals related to eolian deposition. The well-preserved laminated sequence indicates predominant anoxic conditions in the basin floor. Depositional environment had a dominant supply of pluvial detrital sediments and eolian fimaterial with less abundant biogenic input.

  3. Associations of major and trace components in time-series settling particle samples from Cuenca Alfonso, SW Gulf of California

    Science.gov (United States)

    Rodríguez-Castañeda, A. P.; Shumilin, E.; Silverberg, N.; Morton-Bermea, O.; Hernandez-Alvarez, E.; Aguirre-Bahena, F.

    2007-12-01

    Cuenca Alfonso is a natural sedimentation basin in Bahía de La Paz, southern Baja California Peninsula, an arid subtropical region characterized by limited land runoff with a productive surface layer overlying a well-developed Oxygen Minimum Zone. A time-series sediment trap program was initiated in 2002 to help understand the processes controlling variations in the biogeochemistry of this environment. INAA, ICP-MS and ICP-OES analyses, as well as flame AAS were made for major and trace elements in 105 subsamples of material collected at 350 m depth during 2002-2005. Principal component analysis, including data for organic and inorganic carbon, biogenic silica and the lithogenic fraction, yielded four factors. Factor 1 (25% of the total variance) showed high eigenvalues for the classical terrigenous aluminosilicate elements: Al, Fe, Mn Sc. High loadings also occurred for the group of light to medium REEs (except for Eu). The latter are frequently associated with acid source rocks, such the granites and rhyolitic volcanics exposed on the margin of the bay. Factor 2 (18%) grouped mainly REEs, with high loading on the heavier members of the series that are more typical of basic rocks (thick sequences of andesitic volcanics occur to the NW), as well as Ni and Rb. Factor 3 (12%) appears to represent carbonate organism production, with high loadings for Cinorg, Ca and moderate levels for Corg and Cu, while %litho is moderately negative, as is biogenic silica. The fourth factor (9%) is characterized by high negative loadings for Cd, Co, Se and moderately negative values for Corg. Moderate positive loadings occur only for Sr and, at lower levels, for U, Sb and %lithogenic. This suggests that this grouping is related to particles that have been partially transformed within the Oxygen Minimum Zone. The results will be examined for distinctive periods within the time-series, such as the hurricane-influenced months of August-September 2003, the generally very low fluxes

  4. Gulf Coast Basins and Uplifts [gcstructsg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — These data provide generalized outlines of major basins and uplifts in the Gulf Coast region modified after Plate 2, Principal structural features, Gulf of Mexico...

  5. Cretaceous Onlap, Gulf of Mexico Basin [cretonlapg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The maximum extent of Cretaceous onlap is generalized from Plate 3, Structure at the base and subcrop below Mesozoic marine section, Gulf of Mexico Basin (compiled...

  6. Orogenic Thrust Belt, Gulf of Mexico Basin [gcthrustbg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — These data provide the general location of the Ouachita and Appalachian structural fronts slightly modified from Plate 4, Natural resources, Gulf of Mexico Basin...

  7. Seismic stratigraphic framework of deep central Gulf of Mexico basin

    Energy Technology Data Exchange (ETDEWEB)

    Shaub, F.J.; Buffler, R.T.; Parsons, J.G.

    1984-11-01

    The deep Gulf of Mexico basin is underlain by up to 10 km (33,000 ft) of Jurassic(.) to Holocene layered sedimentary rocks. The multichannel reflection seismic record from the deep Gulf of Mexico was divided into six seismic stratigraphic units for study of the geologic history of this accumulation. The basal Challenger unit (Jurassic (.) to middle Cretaceous) is considered coeval with early basin formation. We interpret it as a deep marine sequence overlying oceanic crust in the central basin and as continental and shallow through deep marine rocks, including thick evaporites, over adjacent transitional crust. The next three units, Campeche, Lower Mexican Ridges and Upper Mexican Ridges, indicate that from the Late Cretaceous through middle Miocene the basin filled progressively from the west and north, most probably with siliceous turbidites interlayered with pelagic deposits. By the late Tertiary, however, salt and shale deformation within thick sedimentary sections along the western and northern margins trapped much of the incoming sediment supply on the shelves and upper slopes. The late Miocene to Pliocene Cinco de Mayo unit, therefore, represents a relatively starved interval. In contrast, the uppermost, or Sigsbee unit, includes the Mississippi Fan, an accumulation up to 3 km (10,000 ft) thick of mainly mass-transported deposits that bypassed the shelf and slope and were deposited directly onto the abyssal plain. In the western and southwestern portions of the deep basin, beyond the fan pinchout, the Pleistocene section is largely a continuation of the Pliocene suspension deposits.

  8. Messinian Events: View from the Provence Basin (Gulf of Lion,Western Mediterranean)

    OpenAIRE

    Bache, François; Gorini, C.; Olivet, Jean-Louis; Rabineau, Marina; Aslanian, Daniel; Suc, J.p.

    2009-01-01

    Though the late Miocene "Messinian Salinity Crisis" has been intensely researched along the circum- Mediterranean basins, few studies have focused on the central part of the Mediterranean Basin and, especially, the pre-salt deposits. Within the Western Mediterranean, the Gulf of Lion is exceptional in that its sedimentary strata have not been significantly deformed. In addition, the Gulf of Lion is characterized by a relatively constant subsidence with continuous accommodation space for sedim...

  9. Comparison of Kuqa foreland basin with Persian Gulf Basin in salt tectonics

    Institute of Scientific and Technical Information of China (English)

    Guimei WAN; Liangjie TANG; Wenzheng JIN

    2007-01-01

    Compared Kuqa foreland basin with Persian Gulf Basin in development of salt layers, salt tectonics, and the relation between salt tectonics and hydrocarbon, it is concluded that the salt diapirs are relative to hydrocarbon. Searching salt diapirs and related traps in Kuqa foreland basin is important. The forming mechanism of salt tectonic in Kuqa foreland basin is different from that of Hormuz Series, but similar to that of Lower Fars Series/Gachsaran Formation. Inspired by the role of salt tectonics of Lower Fars Series/Gachsaran Formation in hydrocarbon accumulation, the authors considered that the exploration below salt layer should be enforced, and the traps below salt layer in the southern part of the Kuqa foreland basin would be found where salt layer is thicker. On the contrary, the traps should be found both above and below the salt layer in front of the northern mountain where salt layer is thin. The Triassic and Jurassic source rocks are rich in this area with great exploration prospective.

  10. Post Mid-Cretaceous seismic stratigraphy and geologic history, deep Gulf of Mexico basin

    Energy Technology Data Exchange (ETDEWEB)

    Feng Jianhua; Buffler, R.T. (Univ. of Texas, Austin (United States))

    1991-03-01

    The deep Gulf of Mexico basin is underlain by up to 10 km of sedimentary rocks. This section is subdivided into two megasequences separated by a prominent, basinwide, mid-Cretaceous sequence boundary (MCSB), which marks a major turning point in the history of the Gulf basin. The post-MCSB section consists of the more distal portions of large siliciclastic wedges that partially fill the basin. A detailed seismic stratigraphic analysis has subdivided the post-MCSB, pre-Pleistocene section into 12 new sequences, which have been mapped throughout the entire deep basin using UTIG and all available industry seismic data. Correlation with two published Exxon seismic lines on the northeastern shelf provides tentative age control for the five youngest sequences. The correlation across the slope was made using a dense grid of UTIG and industry seismic data with minimum interference from salt structures. These ages were further confirmed by correlation with DSDP sites 90 and 91 in the western Gulf. This study suggests that the base of the Mississippi Fan is Upper miocene in age, which is older than the Plio-Pleistocene age proposed by previous studies. Isopach maps of each new sequence document the progressive filling of the deep basin and the shift of major deep water depocenters from the west and northwest to the north. This corresponds to the shift of the deltaic depocenters along the northern Gulf margin. A tentative correlation of the deep Gulf sequences with the major northern Gulf coast depositional episodes is proposed.

  11. Morphology and Late Quaternary sedimentation in the Gulf of Oman Basin

    Science.gov (United States)

    Uchupi, Elazar; Swift, S. A.; Ross, D. A.

    The morphology of the Gulf of Oman Basin, a 3,400 m deep oceanic basin between Oman and southern Pakistan and southern Iran, ranges from a convergent margin (Makran margin) along the north side, a passive type (Oman margin) along the south side, translation types along the basin's west (Zendan Fault-Oman Line) and east (Murray Ridge) sides and a narrow continental rise and a wide abyssal plain in the centre of the basin. Sediment input into the basin during the Late Quaternary has been mainly from the north as a result of the uplift of the Coast Makran Mountains in the Late Miocene-Pliocene. Today most of this detritrus is deposited on the shelf and upper continental slope and perched basins behind the fold/fault ridges on the lower slope. The presence of fans and channels on the continental rise on the north side of the basin indicate, however, that continental derived debris was, and possibly is, being transported to the deep-sea by turbidity currents via gaps in the ridges on the lower slope. In addition to land derived terrigenous sediments, the basin deposits also contain biogenic (organic matter and calcium carbonate), eolian detritus and hydrates and authigenic carbonates from the tectonic dewatering of the Makran accretionary wedge. The eolian sediment is carried into the Gulf of Oman Basin from Arabia and the Mesopotamia Valley by the northwesterly Shamal winds. This type of detritus was particularly abundant during the glacial arid periods 21,000-20,000 and 11,000 (Younger Dryas) years ago when exposure of the Persian (Arabian) Gulf increased the area of dust entrainment and shifted the position of the source of the eolian sediments closer to the basin.

  12. Tectonoestratigraphic and Thermal Models of the Tiburon and Wagner Basins, northern Gulf of California Rift System

    Science.gov (United States)

    Contreras, J.; Ramirez Zerpa, N. A.; Negrete-Aranda, R.

    2014-12-01

    The northern Gulf of California Rift System consist sofa series faults that accommodate both normal and strike-slip motion. The faults formed a series of half-greens filled with more than 7 km of siliciclastic suc­cessions. Here, we present tectonostratigraphic and heat flow models for the Tiburón basin, in the southern part of the system, and the Wag­ner basin in the north. The models are constrained by two-dimensional seis­mic lines and by two deep boreholes drilled by PEMEX­-PEP. Analysis of the seismic lines and models' results show that: (i) subsidence of the basins is controlled by high-angle normal faults and by flow of the lower crust, (ii) basins share a common history, and (iii) there are significant differences in the way brittle strain was partitioned in the basins, a feature frequently observed in rift basins. On one hand, the bounding faults of the Tiburón basin have a nested geometry and became active following a west-to-east sequence of activation. The Tiburon half-graben was formed by two pulses of fault activity. One took place during the protogulf extensional phase in the Miocene and the other during the opening of Gulf of California in the Pleistocene. On the other hand, the Wagner basin is the result of two fault generations. During the late-to middle Miocene, the west-dipping Cerro Prieto and San Felipe faults formed a domino array. Then, during the Pleistocene the Consag and Wagner faults dissected the hanging-wall of the Cerro Prieto fault forming the modern Wagner basin. Thermal modeling of the deep borehole temperatures suggests that the heat flow in these basins in the order of 110 mW/m2 which is in agreement with superficial heat flow measurements in the northern Gulf of California Rift System.

  13. Seismic stratigraphy of middle Cretaceous unconformity (MCU) in central Gulf of Mexico basin

    Energy Technology Data Exchange (ETDEWEB)

    Faust, M.J.

    1986-05-01

    A widespread high-amplitude reflector seen on seismic data throughout the Gulf of Mexico has been called the middle Cretaceous unconformity (MCU). This reflector seems to be a major stratigraphic boundary in the Gulf of Mexico basin. It is believed to correspond to Vail's type 1 unconformity of middle Cenomanian age (97 Ma), which records an eustatic drop in sea level of approximately 200 m. This study area includes the entire Gulf of Mexico, except areas of thick, highly deformed salt where following the MCU with any degree of confidence becomes impossible. The MCU is easy to follow in multichannel seismic reflection profiles collected by the Institute for Geophysics of the University of Texas at Austin in the Gulf of Mexico. In central, deeper part of the gulf, reflectors above and below the MCU are parallel. In the southern and eastern rims of the gulf, along the Campeche and Florida escarpments, reflectors are truncated below the MCU and show onlap relationships above it. Therefore, the MCU may be interpreted as representing an unconformity along the southern and eastern rims of the Gulf of Mexico basin. The unconformity appears to die out and grade into a conformable section toward the center of the basin, and channeling is common along the Campeche and Florida escarpments. These channels can be projected back into canyons in the escarpments, which were probably initiated by subaerial exposure of the top of the escarpments during the middle Cretaceous lowstand. The downslope channels, being sourced by the canyons, were cut in deep water.

  14. Geophysical observations on northern part of Georges Bank and adjacent basins of Gulf of Maine

    Science.gov (United States)

    Oldale, R.N.; Hathaway, J.C.; Dillon, William P.; Hendricks, J.D.; Robb, James M.

    1974-01-01

    Continuous-seismic-reflection and magnetic-intensity profiles provide data for inferences about the geology of the northern part of Georges Bank and the basins of the Gulf of Maine adjacent to the bank. Basement is inferred to be mostly sedimentary and volcanic rocks of Paleozoic age that were metamorphosed and intruded locally by felsic and mafic plutons near the end of the Paleozoic Era. During Late Triassic time, large fault basins formed within the Gulf of Maine and probably beneath Georges Bank. The fault basins and a possible major northeast-trending fault zone beneath the northern part of the bank probably formed as a result of the opening Atlantic during the Mesozoic. Nonmarine sediments, associated with mafic flows and intrusive rocks, were deposited in the fault basins as they formed. The upper surface of the Triassic and pre-Triassic rocks that comprise basement is an unconformity that makes up much of the bottom of the Gulf of Maine. Depth to the basement surface beneath the gulf differ greatly because of fluvial erosion in Tertiary time and glacial erosion in Pleistocene time. Beneath the northern part of Georges Bank the basement surface is smoother and slopes southward. Prominent valleys, cut before Late Cretaceous time, are present beneath this part of the bank. Cretaceous, Tertiary, and possibly Jurassic times were characterized by episodes of coastal-plain deposition and fluvial erosion. During this time a very thick wedge of sediment, mostly of Jurassic(?) and Cretaceous ages, was deposited on the shelf. Major periods of erosion took place at the close of the Cretaceous and during the Pliocene. Fluvial erosion during the Pliocene removed much of the coastal-plain sedimentary wedge and formed the Gulf of Maine. Pleistocene glaciers eroded all but a few remnants of the coastal-plain sediments within the gulf and deposited a thick section of drift against the north slope of Georges Bank and a thin veneer of outwash on the bank. Marine sediments were

  15. Differences in phosphorus and nitrogen delivery to the Gulf of Mexico from the Mississippi River Basin

    Science.gov (United States)

    Alexander, R.B.; Smith, R.A.; Schwarz, G.E.; Boyer, E.W.; Nolan, J.V.; Brakebill, J.W.

    2008-01-01

    Seasonal hypoxia in the northern Gulf of Mexico has been linked to increased nitrogen fluxes from the Mississippi and Atchafalaya River Basins, though recent evidence shows that phosphorus also influences productivity in the Gulf. We developed a spatially explicit and structurally detailed SPARROW water-quality model that reveals important differences in the sources and transport processes that control nitrogen (N) and phosphorus (P) delivery to the Gulf. Our model simulations indicate that agricultural sources in the watersheds contribute more than 70% of the delivered N and P. However, corn and soybean cultivation is the largest contributor of N (52%), followed by atmospheric deposition sources (16%); whereas P originates primarily from animal manure on pasture and rangelands (37%), followed by corn and soybeans (25%), other crops (18%), and urban sources (12%). The fraction of in-stream P and N load delivered to the Gulf increases with stream size, but reservoir trapping of P causes large local- and regional-scale differences in delivery. Our results indicate the diversity of management approaches required to achieve efficient control of nutrient loads to the Gulf. These include recognition of important differences in the agricultural sources of N and P, the role of atmospheric N, attention to P sources downstream from reservoirs, and better control of both N and P in close proximity to large rivers. ?? 2008 American Chemical Society.

  16. Alfonso Reyes y el cine del porvenir

    OpenAIRE

    Betina Keizman

    2015-01-01

    Este artículo se propone situar la reflexión de Alfonso Reyes sobre el cine en el marco de las recepciones del primer cine, considerando también cómo esta reflexión se articula en relación con el pensamiento crítico del escritor mexicano. En particular, se analiza el modo en que, por vía de la especulación, Reyes ensaya posibles redefiniciones para una nueva distribución de lo sensible y de las artes, de los valores cognitivos y expresivos de la luz y de los vínculos arte-ciencia. Lo que se l...

  17. Alfonso Reyes y el cine del porvenir

    Directory of Open Access Journals (Sweden)

    Betina Keizman

    2015-07-01

    Full Text Available Este artículo se propone situar la reflexión de Alfonso Reyes sobre el cine en el marco de las recepciones del primer cine, considerando también cómo esta reflexión se articula en relación con el pensamiento crítico del escritor mexicano. En particular, se analiza el modo en que, por vía de la especulación, Reyes ensaya posibles redefiniciones para una nueva distribución de lo sensible y de las artes, de los valores cognitivos y expresivos de la luz y de los vínculos arte-ciencia. Lo que se lee en Reyes es un esfuerzo por pensar nuevas formas de inventiva que se desprenden (o podrían desprenderse del arte cinematográfico.

  18. La conquista de Niebla por Alfonso X

    OpenAIRE

    García Sanjuán, Alejandro

    2000-01-01

    La conquista de Niebla en 660 H/1262 d.n.e. por el rey Alfonso X (1252-1284) puso fin a los cinco siglos y medio de Historia andalusí de dicha ciudad, largo período iniciado desde su sumisión por `Abd al- c Aziz b. Milsá en 94/713, al comienzo de la irrupción islámica en la Península Ibérica. Se trata, por lo tanto, de un episodio de gran relevancia en el devenir histórico de esta localidad, que ya desde época visigoda fue el principal núcleo urbano del territorio onubens...

  19. Stratigraphical links between Miocene Alpine Foreland basin and Gulf of Lion Passive Margin during lowstands

    Science.gov (United States)

    Rubino, Jean-Loup; Gorini, Christian; Leroux, Estelle; Aslanian, Daniel; Rabineau, Marina; Parize, Olivier; Besson, David

    2015-04-01

    Miocene peri-alpine foreland basin is connected toward the south with the Gulf of Lion passive margin and is predominantly filled by marine shallow water molassic deposits ranging from lower Miocene to Pliocene in age. Nine to ten depositional sequences are recorded and partly preserved in this basin and can be traced into the post rift part of the Gulf of Lion. One of the most surprising feature of the stratigraphic infill is the total lack of lowstand deposits within the foreland basin ; All superimposed sequences only includes transgressive and highstand System Tracts separated by erosional sequence boundaries and the development of incised valley networks filled by tidal deposits during transgression; Besson et al. 2005. It means that the entire foreland basin in SE France is exposed during lowstand periods without any preservation of fluvial deposits. By place few forced regression wedges are preserved at the transition between the foreland and the passive margin, close to the present day coastline. To date no real lowstand wedges have never been reported in the offshore of the Gulf of Lion. A reinterpretation of the best old vintage 2D dip seismic profiles along the passive margin validates the idea that the foreland basin is entirely exposed as well as the proximal part of the passive margin; first because some incised valleys can be occasionally picked on the shelf and second mainly because well defined superimposed or juxtaposed prograding lowstand wedges with nicely defined clinoforms onlapping the sequence boundaries can be recognized on the distal part of the shelf from the Burdigalian to the Messinian. Their ages being constrains by the Calmar well calibration. Unfortunately, they can't be continuously mapped all along the shelf break because of the strong erosion related to the Messinian Unconformity and the associated huge sea level fall.So we have to explain why during the lowstands, exceptionally long fluvial valley networks (more than 300km) can

  20. Persistent Localized Microseism Source in Kyushu Island, North Fiji basin and Gulf of Guniea

    Science.gov (United States)

    Zeng, X.; Xia, Y.; Ni, S.; Shi, Y.

    2012-12-01

    The ambient noise tomography (ANT) has been widely applied to investigating crust and upper mantle seismic structure on different scales. The assumptions (diffusivity of noise wave field, homogeneity of noise sources etc) in the validity of ANT are different from realistic ambient noises which leads to studies about microseism source distribution and excitation mechanism. Most microseism in the band of 1s-100s is considered to be generated in ocean by nonlinear interaction between atmosphere, ocean and solid Earth. Besides such sources, the monochromic signals observed in regional and global seismic networks which are excited by persistent localized (PL) sources also play important role in ANT study. The Noise Cross-correlation Function provides opportunity to detect weak microseism signal generated by localized sources. We report a new 10s PL source in Kyushu Island, Japan to interpret strong precursor signals in NCFs between East Asia seismic stations. The 26s microseism signals in NCFs are employed to investigate source location in Gulf of Guinea and Fiji basin. Difference in location, spectrum and temporal variation support an independent 26s microseism source which situates in North Fiji basin. Narrow band-passed NCFs also reveal twin 26s microseism sources in Gulf of Guinea. Although the excitation mechanism of PL sources is still unclear, the coincidences in location and frequency with volcanic long-period-tremor suggest that magma activity is a potential excitation mechanism of PL sources.

  1. Depositional setting of the Jurassic Haynesville seismic sequence in the Apalachicola Basin, northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Dobson, L.M.; Buffler, R.T. (Univ. of Texas, Austin (USA))

    1990-05-01

    Seismic and well data from the northeastern Gulf of Mexico were used to define the seismic stratigraphy, geologic history, and depositional setting of the Jurassic (Kimmeridgian) Haynesville sequence in the Apalachicola basin. The data show that Haynesville clastic sedimentation updip was coeval with Haynesville carbonate deposition downdip. The regional Jurassic seismic stratigraphic framework includes, in ascending order, the Louann Salt Norphlet-Smackover, Haynesville, and Cotton Valley sequences. In the vicinity of Destin dome, wells have penetrated Haynesville sandstones, shales, and anhydrites. These clastics correlate with low amplitude, low-continuity reflections that characterize the Haynesville over a broad area updip. Similar reflections within the overlying (Tithonian-earliest Berriasian) Cotton Valley clastic sequence make seismic definition of the top Haynesville sequence boundary difficult updip. As Haynesville clastics are replaced by carbonates downdip, a high amplitude reflection marks the top of the sequence. Haynesville carbonates conformably overlie (Oxfordian) Smackover carbonates in the basin center, and the lower sequence boundary cannot be defined where disrupted by growth faults associated with early movement of the (Callovian ) Louann Salt. Sigmoid clinoforms document Haynesville shelf margin development Seismic facies also include oblique clinoforms that prograde eastward into the basin from the Southern Platform and Middle Ground Arch. No wells penetrate this facies. Mapping of the seismic facies and correlation with well data suggest a depositional setting for the Haynesville sequence in which influx of terrigenous clastics probably derived from adjacent land areas to the north and northeast filled a broad lagoon behind a carbonate shelf margin.

  2. Evaluation of area studies of the US Gulf Coast Salt Dome Basins: location recommendation report

    International Nuclear Information System (INIS)

    This document presents the evaluation methodology used for the area characterization studies in salt domes of the interior basins of the Gulf Coast region along with background information on salt domes, the site qualification process, criteria used for dome evaluation, and the technical approach applied. The geologic and environmental data are briefly summarized with reference to pertinent documents that contain details of the area characterization studies. Three recommendations are made as a result of the evaluaton: (1) to eliminate one dome from further study because of a safety flaw; (2) to eliminate three domes from further study for failure to meet site performance criteria; and (3) to continue further studies at the four domes which meet minimum standards for further consideration

  3. Active Atlantic Basin Hurricane Forecast Adds to Concerns About Gulf Oil Spill

    Science.gov (United States)

    Showstack, Randy

    2010-06-01

    During the 6-month Atlantic Basin hurricane season that began on 1 June, there could be between 14 and 23 named storms with top winds of at least 39 miles per hour (mph) in the Gulf of Mexico and Caribbean Sea, according to a forecast issued in late May by the Climate Prediction Center of the National Oceanic and Atmospheric Administration's (NOAA) National Weather Service. The forecast indicates that the named storms could include eight to 14 hurricanes with top winds of at least 74 mph and three to seven major hurricanes with top winds of at least 111 mph. In comparison, the seasonal average is 11 named storms, six hurricanes, and two major hurricanes. The busiest hurricane season on record was 2005, with 28 named storms, including hurricanes Katrina and Rita.

  4. Rock mechanics evaluation of potential repository sites in the Paradox, Permian, and Gulf Coast Basins: Volume 1

    International Nuclear Information System (INIS)

    Thermal and thermomechanical analyses of a conceptual radioactive waste repository containing commercial and defense high-level wastes and spent fuel have been performing using finite element models. The thermal and thermomechanical responses of the waste package, disposal room, and repository regions were evaluated. four bedded salt formations, in Davis and Lavender Canyons in the Paradox Basin of southeastern Utah and in Deaf Smith and Swisher counties in the Permian Basin of northwestern Texas, and three salt domes, Vacherie Dome in northwestern Louisiana and Richton and Cypress Creek Domes in southeastern Mississippi, located in the Gulf Coast Basin, were examined. In the Paradox Basin, the pressure exerted on the waste package overpack was much greater than the initial in situ stress. The disposal room closure was less than 10 percent after 5 years. Surface uplift was nominal, and no significant thermomechanical perturbation of the aquitards was observed. In the Permian Basin, the pressure exerted on the waste package overpack was greater than the initial in situ stress. The disposal room closures were greater than 10 percent in less than 5 years. Surface uplift was nominal, and no significant thermomechanical perturbation of the aquitards was observed. In the Gulf Coast Basin, the pressure exerted on the waste package overpack was greater than the initial in situ stress. The disposal room closures were greater than 10 percent in less than 5 years. No significant thermomechanical perturbation of the overlying geology was observed. 40 refs., 153 figs., 32 tabs

  5. Reconstruction of Sea/Lake-Level Changes in an Active Strike-Slip Basin (Gulf of Cariaco, NE Venezuela)

    Science.gov (United States)

    van Daele, M.; Audemard, F.; Beck, C.; de Batist, M.; van Welden, A.; Moernaut, J.; 2006 Shipboard Party, G.

    2008-05-01

    In January 2006, 76 high-resolution reflection seismic profiles were acquired in the Gulf of Cariaco, Northeast Venezuela. In the upper 100 m of sedimentary infill, 17 unconformity-bounded sequences were identified and mapped throughout the basin. Up to now, no core or borehole information is available to provide age constraints on these units. The sedimentary infill is cut by several faults, Riedel faults in the central part and the El Pilar fault (one of the main faults of the South American-Caribbean plate boundary) in the southern part of the gulf. The connection of the Gulf of Cariaco with the adjacent Cariaco Basin occurs at a present-day water depth of ~ 55 m. This implies that the gulf was disconnected from the world ocean and functioned as a lake during a large part of the last glacial. The main rivers entering the gulf drain the coastal mountain ranges and tend to form pronounced deltas at their inlet. During times when the gulf was a lake, periods with a dry climate resulted in dramatic lake-level lowstands and even complete desiccation/evaporation. The present-day depths of delta offlap breaks and the presence of lowstand/evaporite deposits can thus be used to estimate sea/lake level at the time of their formation. Detailed analysis of these stratigraphic sea/lake-level indicators allowed reconstructing the sea/lake-level history for the period encompassed by the 17 identified sequences. This sea/lake-level reconstruction also needed to be corrected for tectonic subsidence, affecting different parts of the gulf with different intensity. The reconstructed sea/lake-level curve of the Gulf of Cariaco was compared with the eustatic sea-level curve and with results of previous paleoclimate studies in Venezuela. The striking coherence between the eustatic curve and the amplitudes and absolute heights of successive reconstructed lowstands and highstands compelled us to tune our record to the eustatic curve in order to achieve a rough age estimate for our units

  6. Attributes and origins of ancient submarine slides and filled embayments: examples from the Gulf Coast basin

    Science.gov (United States)

    Morton, Robert

    1993-01-01

    Large submarine slides and associated shelf-margin embayments represent an intermediate member in the continuum of unstable shelf-margin features. On seismic profiles, they may resemble submarine canyons, but are different in their size, morphology, origin, and hydrocarbon exploration potential. Two large Neogene submarine slides, located in the northwestern Gulf Coast Basin, formed on the upper slope and flanks of prominent shelf-margin deltas. The basal detachment surface of each slide is a structural discontinuity that may be misinterpreted as an erosional unconformity and, therefore, misidentified as a stratigraphic boundary separating depositional sequences. Regional stratigraphic correlations indicate that both slides were initiated after the continental platform wa flooded. The condensed sections deposited during the rise in relative sea level contain the basal detachment surfaces. Beyond these observations, the relationships between the slides and sea level fluctuations are uncertain. The shelf-margin embayments created by the slides apparently were partly excavated during periods of lowered relative sea level and were filled during the subsequent relative sea level rise and highstand. Eventually the preslide morphology of the shelf margin was restored by coalesced prograding deltas.

  7. Geochemical features of heavy metal bioaccumulation in the Guaymas Basin of the Gulf of California

    Science.gov (United States)

    Demina, L. L.; Galkin, S. V.

    2009-10-01

    Atomic absorption spectroscopy (flame and graphite furnace techniques) and instrumental neutron activation analysis were used for determining the Fe, Mn, Zn, Cu, Pb, Cd, Ag, Co, Cr, As, Se, Sb, Ba, Au, and Hg contents in 25 samples of different tissues and whole organisms inhabiting the southern trough in the Guaymas Basin (Gulf of California) and in several samples of its bottom waters. It is shown that the habitat environment of this hydrothermal field with high primary production of both photosynthetic and bacterial chemosynthetic origin influences the Fe and Mn ratios in the waters of the microbiotopes and the distribution patterns of the metals in the external and internal organs of the benthic animals. In the dominant specialized taxa, the maximal bioaccumulation of metals is registered both in the organs related to bacterial chemosynthesis such as the trophosome of Vestimentifera Riftia pachyptila and the gills of the vesicomyid clam Archivestica gigas and in other organs. The other organisms such as the mollusks Nuculana grasslei, actinias Paraphelliactis pabista, Actinaria, and Spongia and the crabs Munidopsis alvisca demonstrate high bioaccumulation properties as well. The metal concentration coefficient is highly variable ranging from 10 to 104. The changes in the molar Fe/Mn ratio values imply the partitioning of these two metals in the following migration succession: microbiotope water-external organs-internal organs.

  8. High-resolution 3D seismic imaging of a pull-apart basin in the Gulf of Cadiz

    Science.gov (United States)

    Crutchley, G.; Berndt, C.; Klaeschen, D.; Gutscher, M.

    2009-12-01

    In 2006, high-resolution 3D seismic data were acquired in the Gulf of Cadiz and the Mediterranean Sea aboard the RRS Charles Darwin as part of the HERMES (Hotspot Ecosystem Research on the Margins of European Seas) project. The P-Cable system, a cost-efficient set-up for fast acquisition of 3D seismic data on 12 single-channel streamers, was utilized to acquire seismic cubes at four different targets. Here, we present results from the second target - a WNW-ESE-oriented pull-apart basin in the southeastern Gulf of Cadiz. Initial processing has included: 1) spatial positioning of each recording channel from GPS data acquired on the outer two channels, 2) improved positioning of shot points and channels from the inversion of first arrival times, 3) application of a swell filter to improve reflection coherency, 4) CDP binning and stacking and 5) migration. The new data confirm that the southeastern Gulf of Cadiz north of the Rharb submarine valley is structurally controlled by numerous strike slip faults that were active until quite recently (within the resolution of the data). Given the location of this basin, between the extensional domain on the upper slope and the compressional toe of the accretionary wedge, we interpret the origin to be gravitational sliding on a detachment layer, possibly containing salt, but at this stage not imaged by our profiles.

  9. Teorias y critica literaria en la obra de Alfonso Reyes

    OpenAIRE

    Aatar, Abdellah

    2012-01-01

    La obra literaria de Alfonso Reyes marca un momento crucial en la historia de la literatura universal, debido a la pluralidad tematica que pone de relive desde ya los principios del siglo XX? Como es el caso del helenismo, el mexicanismo y la teoria literaria. pero en todos ellos, sobresale el concepto de la teoria literaria y la critica como tema multifascetico que se encuentra en cada uno de los temas excentricos; estableciendo una red de relaciones con lo general y lo particular con el ...

  10. Modern dinocyst assemblages from the Gulf of Mexico: importance of the basin as potential refuge for late Cenozoic species

    Science.gov (United States)

    Limoges, Audrey; de Vernal, Anne; Londeix, Laurent

    2013-04-01

    Surface sediment samples (0-1 cm) from 44 sites of the Gulf of Mexico and adjacent lagoonal bodies were analyzed for their palynological content in order to document the relationship between organic-walled dinoflagellates cysts (dinocysts) and sea-surface conditions (temperature, salinity, productivity). The analyses also aimed at identifying tracers of toxic algal blooms from sedimentary records. According to redundancy analyses (RDA), the distance to the coast and winter temperature are the most important factors that control cyst distribution in sediment from the study area. They explain respectively 53.2 and 18.6% of the total variance. Our results also demonstrate the richness and thermophilic character of the modern dinocyst assemblages from the Gulf of Mexico. They include taxa typical of tropical and subtropical environments, two potentially toxic species (Polysphaeridium zoharyi and Lingulodinium machaerophorum) as well as species that disappeared from the dinocyst flora of the mid-latitudes of the North Atlantic since the Pliocene period. Worth of mention is the presence of Melitasphaeridium choanophorum as a minor component of assemblages from the north and southwestern Gulf of Mexico, although it was considered extinct by the end of the Pleistocene (> 0.011 Ma). This would imply that this species is currently still living in the study area, and suggest that the basin probably acts as sheltered environment fostering the persistence of endemic species.

  11. Seismic imaging and analysis of source and migration within an integrated hydrocarbon system study: Northern Gulf of Mexico Basin

    Energy Technology Data Exchange (ETDEWEB)

    Gross, Oliver P.; Hood, Kenneth C.; Harrison, Stanley C. [Exxon Exploration Co., Houston, TX (United States); Wenger, Lloyd M. [Exxon Production Research Co., Houston, TX (United States)

    1995-12-31

    The sources for hydrocarbons in young Tertiary reservoirs of the offshore Gulf of Mexico have been enigmatic in the past due to the lack of source rock penetration in offshore drilling. Exxon formed a multidisciplinary team to address source, maturation, and migration in the northern Gulf of Mexico. The study was initiated in a pilot area east of the Mississippi River Delta where the complete hydrocarbon system can be seismically imaged, then expanded to the west across much of the shelf and slope. Hydrocarbons from seeps and reservoirs were geochemically characterized across the entire northern Gulf of Mexico Basin, and direct oil to source rock correlations were made both offshore (in pilot area) and onshore. Modern 2-D and 3-D seismic was used to develop a geologic framework and to map potential offshore source intervals. The major sources identified offshore are centered on the Eocene, Turonian, Tithonian, and Oxfordian, and correspond to second-order sequence stratigraphic transgressions. (author). 1 fig., 1 tab

  12. Sr-Nd isotopes constrain on the deposit history of the basins in the Gulf of Mexico

    Science.gov (United States)

    Li, Y.; Jiang, S.

    2015-12-01

    The Brazos-Trinity Basin IV and Ursa Basin are situated on the northern slope of the Gulf of Mexico. The Ursa basin lies in the center of late Pleistocene Mississippi River deposition, received the sediment deposition during Marine Isotope Stage (MIS) 2- 4. The Brazos-Trinity Basin IV belongs to a part of the Brazos-Trinity fan, it recorded the turbidite deposition and hemiplegic deposition during MIS1- 5. The Sr and Nd isotopic composition of the detrital composition of the sediment in both basins indicates the change of the sediment provenance during the basin-filled process. In the Ursa basin, The difference of 87Sr/86Sr ratio and ɛNd of the detrital component between MIS1,2 (87Sr/86Sr ~ 0.7219 - 0.7321, ɛNd ~ -12 - -13.4) and MIS3,4(87Sr/86Sr ~ 0.7310 - 0.7354, ɛNd ~ -16 - -17.9) is suggested to be related with the provenance change of the detrital particles since LGM. The addition of detrital particle from Appalachians with less radiogenic 87Sr/86Sr and positive ɛNd altered the character of the sediment of the Mississippi River during the last glaciation and deglaciation. In the Brazos-Trinity Basin IV, the narrow range of 87Sr/86Sr and ɛNd indicate that the sediment source of Brazos-Trinity Basin IV had not changed obviously during MIS5e to MIS2, mostly from coastal rivers such as Brazos River, Trinity River and Sabine River. The pre-fan with 87Sr/86Sr ~0.735 and ɛNd ~ -14.5 to -16.9, which is very similar to the deep sediment in the Ursa Basin with 87Sr/86Sr ~0.733 to 0.735 and ɛNd ~ -16 to -18. It is suggested that sediments of the pre-fan of the Brazos-Trinity Basin IV were supplied from the ancestral Mississippi River Delta during the low sea level (MIS 6). During the MIS5, the discharge of Mississippi River is thought switched to its present course, ~300 km to the east.

  13. The Cretaceous-Paleogene boundary deposit in the Gulf of Mexico: Large-scale oceanic basin response to the Chicxulub impact

    Science.gov (United States)

    Sanford, Jason C.; Snedden, John W.; Gulick, Sean P. S.

    2016-03-01

    Hydrocarbon exploration in the last decade has yielded sufficient data to evaluate the Gulf of Mexico basin response to the Chicxulub asteroid impact. Given its passive marine setting and proximity to the impact structure on the Yucatán Peninsula, the gulf is the premier locale in which to study the near-field geologic effect of a bolide impact. We mapped a thick (decimeter- to hectometer-scale) deposit of carbonate debris at the Cretaceous-Paleogene boundary that is ubiquitous in the gulf and readily identifiable on borehole and seismic data. We interpret deposits seen in seismic and borehole data in the deepwater gulf to be predominately muddy debrites with minor turbidites based on cores in the southeastern gulf. Mapping of the deposit in the northern Gulf of Mexico reveals that the impact redistributed roughly 1.05 × 105 km3 of sediment therein and over 1.98 × 105 km3 gulfwide. Deposit distribution suggests that the majority of sediment derived from coastal and shallow-water environments throughout the gulf via seismic and megatsunamic processes initiated by the impact. The Texas shelf and northern margin of the Florida Platform were significant sources of sediment, while the central and southern Florida Platform underwent more localized platform collapse. The crustal structure of the ancestral gulf influenced postimpact deposition both directly and indirectly through its control on salt distribution in the Louann Salt Basin. Nevertheless, impact-generated deposition overwhelmed virtually all topography and depositional systems at the start of the Cenozoic, blanketing the gulf with carbonate debris within days.

  14. Formation mechanisms of heavy oils in the Liaohe Western Depression,Bohai Gulf Basin

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    The Liaohe Oilfield in the Liaohe Western Depression of the Bohai Gulf Basin is the third-largest oil producing province and the largest heavy oil producing oilfield in China. A total of 65 oil samples,35 rock samples and 36 reservoir sandstone samples were collected and analyzed utilizing conventional geochemical and biogeochemical approaches to unravel the mechanisms of the formation of the heavy oils. Investigation of the oils with the lowest maturity compared with the oils in the Gaosheng and Niuxintuo oilfields indicates no apparent relation between the maturity and physical properties of the heavy oils. It is suggested that the heavy oil with primary origin is not likely the main mechanism re-sponsible for the majority of the heavy oils in the Liaohe Western Slope. The absence and/or depletion of n-alkanes etc.,with relatively low molecular weight and the occurrence of 25-norhopane series in the heavy oils as well as the relatively high acidity of the oils all suggest that the majority of the heavy oils once experienced secondary alteration. The fingerprints of the total scanning fluorescence (TSF) of the inner adsorbed hydrocarbons on the reservoir grains and the included hydrocarbons in fluid inclusions are similar to that of the normal oils in the area but are different from the outer adsorbed and reser-voired free oils at present,further indicating that most of the heavy oils are secondary in origin. Analyses of bacteria (microbes) in 7 oil samples indicate that anaerobic and hyperthermophilic Ar-chaeoglobus sp. are the dominant microbes relevant to oil biodegradation,which coincides with the shallow commercial gas reservoirs containing anaerobic bacteria derived gas in the Gaosheng and Leijia teotonic belts. The biodegradation most likely occurs at the water/oil interface,where the forma-tion water is essential for microbe removal and nutrient transportation. We think that biodegradation,water washing and oxidization are interrelated and are the main

  15. Flux and sources of nutrients in the Mississippi-Atchafalaya River Basin: Topic 3 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico.

    OpenAIRE

    Goolsby, Donald A.; Battaglin, William A.; Lawrence , Gregory B.; Artz, Richard S.; Aulenbach, Brent T.; Hooper , Richard P.; Keeney, Dennis R.; Stensland, Gary J.

    1999-01-01

    Ths report addresses the following two questions: 1) What are the loads (flux) of nutrients transported from the Mississippi-Atchafalaya River Basin to the Gulf of Mexico, and where do they come from within the basin? 2) What is the relative importance of specific human activities, such as agriculture, point-source discharges, and atmospheric deposition in contributing to these loads? These questions were addressed by first estimating the flux of nutrients from the Mississippi-Atchaf...

  16. Late Quaternary climatic and oceanographic changes in the Northeast Pacific as recorded by dinoflagellate cysts from Guaymas Basin, Gulf of California (Mexico)

    OpenAIRE

    Price, Andrea M; Mertens, Kenneth; Pospelova, Vera; Pedersen, Thomas F; Ganeshram, Raja S.

    2013-01-01

    A high-resolution record of organic-walled dinoflagellate cyst production in Guaymas Basin, Gulf of California (Mexico) reveals a complex paleoceanographic history over the last ~40 ka. Guaymas Basin is an excellent location to perform high resolution studies of changes in late Quaternary climate and paleo-productivity because it is characterized by high primary productivity, high sedimentation rates, and low oxygen bottom waters. These factors contribute to the deposition and preservation of...

  17. Basin Analysis and Petroleum System Characterization and Modeling, Interior Salt Basins, Central and Eastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini; Paul Aharon; Donald A. Goddard; Roger Barnaby

    2006-05-26

    The principal research effort for Phase 1 (Concept Development) of the project has been data compilation; determination of the tectonic, depositional, burial, and thermal maturation histories of the North Louisiana Salt Basin; basin modeling (geohistory, thermal maturation, hydrocarbon expulsion); petroleum system identification; comparative basin evaluation; and resource assessment. Existing information on the North Louisiana Salt Basin has been evaluated, an electronic database has been developed, and regional cross sections have been prepared. Structure, isopach and formation lithology maps have been constructed, and burial history, thermal maturation history, and hydrocarbon expulsion profiles have been prepared. Seismic data, cross sections, subsurface maps and burial history, thermal maturation history, and hydrocarbon expulsion profiles have been used in evaluating the tectonic, depositional, burial and thermal maturation histories of the basin. Oil and gas reservoirs have been found to be associated with salt-supported anticlinal and domal features (salt pillows, turtle structures and piercement domes); with normal faulting associated with the northern basin margin and listric down-to-the-basin faults (state-line fault complex) and faulted salt features; and with combination structural and stratigraphic features (Sabine and Monroe Uplifts) and monoclinal features with lithologic variations. Petroleum reservoirs include Upper Jurassic and Cretaceous fluvial-deltaic sandstone facies; shoreline, marine bar and shallow shelf sandstone facies; and carbonate shoal, shelf and reef facies. Cretaceous unconformities significantly contribute to the hydrocarbon trapping mechanism capacity in the North Louisiana Salt Basin. The chief petroleum source rock in this basin is Upper Jurassic Smackover lime mudstone beds. The generation of hydrocarbons from Smackover lime mudstone was initiated during the Early Cretaceous and continued into the Tertiary. Hydrocarbon

  18. BASIN ANALYSIS AND PETROLEUM SYSTEM CHARACTERIZATION AND MODELING, INTERIOR SALT BASINS, CENTRAL AND EASTERN GULF OF MEXICO

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini; Donald A. Goddard; Ronald K. Zimmerman

    2005-05-10

    The principal research effort for Year 2 of the project has been data compilation and the determination of the burial and thermal maturation histories of the North Louisiana Salt Basin and basin modeling and petroleum system identification. In the first nine (9) months of Year 2, the research focus was on the determination of the burial and thermal maturation histories, and during the remainder of the year the emphasis has basin modeling and petroleum system identification. Existing information on the North Louisiana Salt Basin has been evaluated, an electronic database has been developed, regional cross sections have been prepared, structure and isopach maps have been constructed, and burial history, thermal maturation history and hydrocarbon expulsion profiles have been prepared. Seismic data, cross sections, subsurface maps and related profiles have been used in evaluating the tectonic, depositional, burial and thermal maturation histories of the basin. Oil and gas reservoirs have been found to be associated with salt-supported anticlinal and domal features (salt pillows, turtle structures and piercement domes); with normal faulting associated with the northern basin margin and listric down-to-the-basin faults (state-line fault complex) and faulted salt features; and with combination structural and stratigraphic features (Sabine and Monroe Uplifts) and monoclinal features with lithologic variations. Petroleum reservoirs are mainly Upper Jurassic and Lower Cretaceous fluvial-deltaic sandstone facies and Lower Cretaceous and Upper Cretaceous shoreline, marine bar and shallow shelf sandstone facies. Cretaceous unconformities significantly contribute to the hydrocarbon trapping mechanism capacity in the North Louisiana Salt Basin. The chief petroleum source rock in this basin is Upper Jurassic Smackover lime mudstone beds. The generation of hydrocarbons from Smackover lime mudstone was initiated during the Early Cretaceous and continued into the Tertiary

  19. Basin Analysis and Petroleum System Characterization and Modeling, Interior Salt Basins, Central and Eastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini

    2005-03-31

    The principal research effort for Year 2 of the project is the determination of the burial and thermal maturation histories and basin modeling and petroleum system identification of the North Louisiana Salt Basin. In the first six (6) to nine (9) months of Year 2, the research focus is on the determination of the burial and thermal maturation histories and the remainder of the year the emphasis is on basin modeling and petroleum system identification. No major problems have been encountered to date, and the project is on schedule.

  20. BASIN ANALYSIS AND PETROLEUM SYSTEM CHARACTERIZATION AND MODELING, INTERIOR SALT BASINS, CENTRAL AND EASTERN GULF OF MEXICO

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini

    2004-11-05

    The principal research effort for Year 2 of the project is the determination of the burial and thermal maturation histories and basin modeling and petroleum system identification of the North Louisiana Salt Basin. In the first six (6) to nine (9) months of Year 2, the research focus is on the determination of the burial and thermal maturation histories and the remainder of the year the emphasis is on basin modeling and petroleum system identification. No major problems have been encountered to date, and the project is on schedule.

  1. Imágenes de la "Pasión" en el teatro de Alfonso Sastre

    OpenAIRE

    Aboal Sanjurjo, María Isabel

    2002-01-01

    Presencia bíblica, de la liturgia cristiana, de la divinidad y de lo sacro en la dramaturgia de Alfonso Sastre como elemento vertebrador de la coherencia interna de su teatro a lo largo de toda su trayectoria.

  2. Fluid transport by solitary waves along growing faults. A field example from the South Eugene Island Basin, Gulf of Mexico

    Science.gov (United States)

    Revil, A.; Cathles, L. M.

    2002-09-01

    The Red Fault system is one of the main growth faults found in the South Eugene Island Basin, a salt withdrawal minibasin located offshore Louisiana, in the Gulf of Mexico. This fault system corresponds to a lateral boundary between fluid overpressured compartments. In addition, there is a set of observations indicating that the Red Fault system exhibits rapid episodic migration of fluids. This fault represents an example of preferential pathway for the upward episodic migration of overpressured hydrocarbons from deep, heavily pressured, compartments on time scales of years. The migrations of fluids into active growing faults could take the form of propagating surges (solitary waves) that propagate upward along the fault planes in a wave-like manner at km/yr. Solitary waves represent a very efficient mechanism for the upward transport of fluids along growth faults in sedimentary basins generating its own permeability. In addition, this mechanism is compatible with the fact that the fault plane is observed to sustain a static pore fluid pressure difference between its two sides. The propagation of solitary waves in active growth faults appears as a fundamental mechanism to understand the nature of upward fast migration of fluids along active growth faults in compartimentalized sedimentary basins.

  3. Messinian erosional and salinity crises: View from the Provence Basin (Gulf of Lions, Western Mediterranean)

    OpenAIRE

    Bache, François; Olivet, Jean-Louis; Gorini, Christian; Rabineau, Marina; Baztan, J.; Aslanian, Daniel; Suc, Jean-Pierre

    2009-01-01

    International audience Though the late Miocene “Messinian Salinity Crisis” has been intensely researched along the circum-Mediterranean basins, few studies have focused on the central part of the Mediterranean Basin and, especially, the pre-salt deposits. To improve our knowledge of the Messinian events, it is imperative to better understand this domain. In this study, we provide a more complete understanding of this central domain in the Provence Basin. We were able to recognize: a) thick...

  4. Sequence stratigraphy and high-frequency cycles: New aspects for a quantitative evaluation of the Gulf of Suez basin, Egypt

    Energy Technology Data Exchange (ETDEWEB)

    Nio, S.D.; Yang, C.S. (International Geoservices, Leiderdorp (Netherlands)); Tewfik, N.; Darwish, M. (Earth Resource Exploration, Cairo (Egypt)); Jonkman, H. (International Geoservices, Leiderdorp (Netherlands))

    1993-09-01

    A new development in the application of sequence stratigraphic concepts in marine as well as continental basins is the recognition of high-frequency cyclic patterns in rock successions in the subsurface. Studies of six wells from the northern, central, and southern parts of the Gulf of Suez show the presence of well-preserved, high-frequency cycles with periodicities similar to the orbitally forced Malankovitch parameters. Subsurface rock successions, third-order sequences, and high-frequency cycles were compared with outcrops. After establishing the biostratigraphic framework for the above-mentioned wells, a sequence analysis was performed. Sequence boundaries and maximum flooding positions in each well were calibrated with the occurrences and evaluation of the high-frequency cycles. It became obvious that there is an intimate relationship between these high-frequency Milankovitch cycles and sequence organization. In addition, a close relationship can be observed in the subsurface as well as in outcrops between high-frequency climatic changes (connected to the Milankovitch cycles) and (litho)facies variability. Quantitative evaluations of each sequence and/or systems tract can be computed with the International Geoservices' cyclicity analysis tool (MILABAR). The results are summarized in a well composite chart, rate (NAR), and ratio of preserved time. In correlations between the wells, an accuracy of 500-100 Ka can be obtained. The quantitative evaluation of the sequence and high-frequency cycle analysis gave some new aspects concerning the (litho)facies and geodynamic development during the pre- as well as the synrift stages of the Gulf of Suez Basin.

  5. Multiple evidence for methylotrophic methanogenesis as the dominant methanogenic pathway in hypersaline sediments from the Orca Basin, Gulf of Mexico

    Science.gov (United States)

    Zhuang, Guang-Chao; Elling, Felix J.; Nigro, Lisa M.; Samarkin, Vladimir; Joye, Samantha B.; Teske, Andreas; Hinrichs, Kai-Uwe

    2016-08-01

    Among the most extreme habitats on Earth, dark, deep, anoxic brines host unique microbial ecosystems that remain largely unexplored. As the terminal step of anaerobic degradation of organic matter, methanogenesis is a potentially significant but poorly constrained process in deep-sea hypersaline environments. We combined biogeochemical and phylogenetic analyses with incubation experiments to unravel the origin of methane in the hypersaline sediments of Orca Basin in the northern Gulf of Mexico. Substantial concentrations of methane, up to 3.4 mM, coexisted with high concentrations of sulfate from 16 to 43 mM in two sediment cores retrieved from the northern and southern parts of Orca Basin. The strong depletion of 13C in methane (-77‰ to -89‰) points towards a biological source. While low concentrations of competitive substrates limited the significance of hydrogenotrophic and acetoclastic methanogenesis, the presence of non-competitive methylated substrates (methanol, trimethylamine, dimethyl sulfide, dimethylsulfoniopropionate) supported the potential for methane generation through methylotrophic methanogenesis. Thermodynamic calculations demonstrated that hydrogenotrophic and acetoclastic methanogenesis were unlikely to occur under in situ conditions, while methylotrophic methanogenesis from a variety of substrates was highly favorable. Likewise, carbon isotope relationships between methylated substrates and methane suggested methylotrophic methanogenesis was the major source of methane. Stable and radio-isotope tracer experiments with 13C-labeled bicarbonate, acetate and methanol and 14C-labeled methylamine indicated that methylotrophic methanogenesis was the predominant methanogenic pathway. Based on 16S rRNA gene sequences, halophilic methylotrophic methanogens related to the genus Methanohalophilus dominated the benthic archaeal community in the northern basin and also occurred in the southern basin. High abundances of methanogen lipid biomarkers such as

  6. LANDSCAPE ECOLOGY ASSESSMENT OF THE TENSAS RIVER BASIN, MISSISSIPPI RIVER DELTA REGION, AND GULF OF MEXICO

    Science.gov (United States)

    A group of landscape ecological indicators were applied to biophysical data masked to the Tensas River Basin. The indicators were use to identify and prioritize sources of nutrients in a Mississippi River System sub-basin. Remotely sensed data were used for change detection a...

  7. Postglacial development of the eastern Gulf of Finland: from Pleistocene glacial lake basins to Holocene lagoon systems

    Science.gov (United States)

    Ryabchuk, Daria; Sergeev, Alexander; Kotilainen, Aarno; Hyttinen, Outi; Grigoriev, Andrey; Gerasimov, Dmitry; Anisimov, Mikhail; Gusentsova, Tatiana; Zhamoida, Vladimir; Amantov, Aleksey; Budanov, Leonid

    2016-04-01

    Despite significant amount of data, there are still lots of debatable questions and unsolved problems concerning postglacial geological history of the Eastern Gulf of Finland, the Baltic Sea. Among these problems are: 1) locations of the end moraine and glacio-fluvial deposits; 2) time and genesis of the large accretion forms (spits, bars, dunes); 3) basinwide correlations of trangression/regression culminations with the other parts of the Baltic Sea basin; 4) study of salinity, timing, frequency and intensity of Holocene saline water inflows and their links of sedimentation processes associated with climate change. Aiming to receive new data about regional postglacial development, the GIS analyses of bottom relief and available geological and geophysical data was undertaken, the maps of preQuaternary relief, moraine and Late Pleistocene surfaces, glacial moraine and Holocene sediments thicknesses were compiled. High-resolution sediment proxy study of several cores, taken from eastern Gulf of Finland bottom, allows to study grain-size distribution and geochemical features of glacial lake and Holocene sediments, to reveal sedimentation rates and paleoenvironment features of postglacial basins. Interdisciplinary geoarcheological approaches offer new opportunities for studying the region's geological history and paleogeography. Based on proxy marine geological and coastal geoarcheological studies (e.g. off-shore acoustic survey, side-scan profiling and sediment sampling, on-shore ground-penetrating radar (GPR SIR 2000), leveling, drilling, grain-size analyses and radiocarbon dating and archeological research) detailed paleogeographical reconstruction for three micro-regions - Sestroretsky and Lahta Lowlands, Narva-Luga Klint Bay and Southern Ladoga - were compiled. As a result, new high resolution models of Holocene geological development of the Eastern Gulf of Finland were received. Model calibration and verification used results from proxy geoarcheological research

  8. Structure of the Wagner Basin in the Northern Gulf of California From Interpretation of Seismic Reflexion Data

    Science.gov (United States)

    Gonzalez, M.; Aguilar, C.; Martin, A.

    2007-05-01

    The northern Gulf of California straddles the transition in the style of deformation along the Pacific-North America plate boundary, from distributed deformation in the Upper Delfin and Wagner basins to localized dextral shear along the Cerro Prieto transform fault. Processing and interpretation of industry seismic data adquired by Petroleos Mexicanos (PEMEX) allow us to map the main fault structures and depocenters in the Wagner basin and to unravel the way strain is transferred northward into the Cerro Prieto fault system. Seismic data records from 0.5 to 5 TWTT. Data stacking and time-migration were performed using semblance coefficient method. Subsidence in the Wagner basin is controlled by two large N-S trending sub-parallel faults that intersect the NNW-trending Cerro Prieto transform fault. The Wagner fault bounds the eastern margin of the basin for more than 75 km. This fault dips ~50° to the west (up to 2 seconds) with distinctive reflectors displaced more than 1 km across the fault zone. The strata define a fanning pattern towards the Wagner fault. Northward the Wagner fault intersects the Cerro Prieto fault at 130° on map view and one depocenter of the Wagner basin bends to the NW adjacent to the Cerro Prieto fault zone. The eastern boundary of the modern depocenter is the Consag fault, which extends over 100 km in a N-S direction with an average dip of ~50° (up to 2s) to the east. The northern segment of the Consag fault bends 25° and intersects the Cerro Prieto fault zone at an angle of 110° on map view. The acoustic basement was not imaged in the northwest, but the stratigraphic succession increases its thickness towards the depocenter of the Wagner basin. Another important structure is El Chinero fault, which runs parallel to the Consag fault along 60 km and possibly intersects the Cerro Prieto fault to the north beneath the delta of the Colorado River. El Chinero fault dips at low-angle (~30°) to the east and has a vertical offset of about 0

  9. Resource Assessment of the In-Place and Potentially Recoverable Deep Natural Gas Resource of the Onshore Interior Salt Basins, North Central and Northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini; Donald A. Goddard

    2005-04-15

    The principal research effort for the first six months of Year 2 of the project has been petroleum system characterization. Understanding the burial and thermal maturation histories of the strata in the onshore interior salt basins of the North Central and Northeastern Gulf of Mexico areas is important in petroleum system characterization. The underburden and overburden rocks in these basins and subbasins are a product of their rift-related geohistory. Petroleum source rock analysis and thermal maturation and hydrocarbon expulsion modeling indicate that an effective regional petroleum source rock in the onshore interior salt basins, the North Louisiana Salt Basin, Mississippi Interior Salt Basin, Manila Subbasin and Conecuh Subbasin, was the Upper Jurassic Smackover lime mudstone. The Upper Cretaceous Tuscaloosa shale was an effective local petroleum source rock in the Mississippi Interior Salt Basin and a possible local source bed in the North Louisiana Salt Basin. Hydrocarbon generation and expulsion was initiated in the Early Cretaceous and continued into the Tertiary in the North Louisiana Salt Basin and the Mississippi Interior Salt Basin. Hydrocarbon generation and expulsion was initiated in the Late Cretaceous and continued into the Tertiary in the Manila Subbasin and Conecuh Subbasin. Reservoir rocks include Jurassic, Cretaceous and Tertiary siliciclastic and carbonate strata. Seal rocks include Jurassic, Cretaceous and Tertiary anhydrite and shale beds. Petroleum traps include structural and combination traps.

  10. "De arauigo en lenguaie castellano": Politica linguistica e traduzione secondo Alfonso X

    Directory of Open Access Journals (Sweden)

    Ruggiero Pergola

    2015-07-01

    Full Text Available Abstract – After Alfonso X’s accession to the throne in mid-13th-century Spain, the translating activity of scientific texts from Arabic changed route: Castilian, instead of Latin, became the language of science. Such a plan, ambitious though risky, was carried out through the writing of the huge Alfonsine corpus of texts, a fundamental contribution to medieval culture, which shaped the picture of Alfonso as “Emperor of Culture”. The aim of this paper is to provide, in the light of recent research, an overall view of the main translators and of the translations of scientific texts from Arabic into Castilian at Alfonso’s court.Abstract – Con l’avvento di Alfonso X nella Spagna della metà del XIII secolo, l’attività traduttiva di testi scientifici dall’arabo conobbe un significativo cambio di rotta: il passaggio dal latino al castigliano come lingua scientifica. Il progetto, ambizioso e rischioso, si realizzò nella redazione dell’immenso corpus alfonsino, fondamentale contributo alla cultura medievale, che ha creato l’immagine di Alfonso “imperatore della cultura”. Obiettivo di questo contributo è offrire, alla luce degli studi più recenti, una visione d’insieme sui principali traduttori e sulle traduzioni di testi scientifici dall’arabo in castigliano realizzate alla corte di Alfonso X.

  11. Structure and Stratigraphy of the Rift Basins in the Northern Gulf of California: Results from Analysis of Seismic Reflection and Borehole Data.

    Science.gov (United States)

    Martín, A.; González, M.; Helenes, J.; García, J.; Aragón, M.; Carreño, A.

    2008-12-01

    The northern Gulf of California contains two parallel, north-south trending rift basin systems separated by a basement-high. The interpretation of several exploration wells, and ~4500 km of seismic reflection data from PEMEX (Mexican national oil company) indicate that the tectonically active basins to the west (Wagner- Consag and Upper Delfin basins) may have initiated synchronously with the now abandoned Tiburón- Tepoca-Altar basins to the east in the Sonora margin. In both basin systems the lower sequence (A) is marine mudstone-siltstone, has parallel reflectors and a largely uniform thickness that reaches up to1.5 km, and gradually pinches out toward the lateral margins. This suggests that the unit was deposited prior to their segmentation by transtensional faulting. Marine microfossils from borehole samples from sequence A in the Tiburón and Consag basins indicates middle Miocene (>11.2 Ma) proto-Gulf conditions. Sequence B conformably overlies sequence A, and is characterized by up to 2 km growth strata with a fanning geometry that show a clear genetic relationship to the major transtensional faults that control the segmentation of the two basin systems. Sequence C in the Tiburón and Tepoca basins is comparatively thin (<800 m) and includes several unconformities, but is much less affected by faulting. In contrast, sequence C in the active Wagner, Consag and Upper Delfin basin is a much thicker (up to 2 km) growth sequence with abundant volcanic intrusions. Marked variations in sequence C in the different basin systems clearly demonstrate a major westward shift of deformation and subsidence at this time. The modern depocenter in Wagner-Consag basins is controlled by the Consag and Wagner faults, which trend parallel to the north ~20 km apart, and show opposite normal offset. These two faults merge at an oblique angle (70°-50°, respectively) into the Cerro Prieto transform fault to the north and likely accommodate an important amount of dextral shear. To

  12. Targeted technology applications for infield reserve growth: A synopsis of the Secondary Natural Gas Recovery project, Gulf Coast Basin. Topical report, September 1988--April 1993

    Energy Technology Data Exchange (ETDEWEB)

    Levey, R.A.; Finley, R.J.; Hardage, B.A.

    1994-06-01

    The Secondary Natural Gas Recovery (SGR): Targeted Technology Applications for Infield Reserve Growth is a joint venture research project sponsored by the Gas Research Institute (GRI), the US Department of Energy (DOE), the State of Texas through the Bureau of Economic Geology at The University of Texas at Austin, with the cofunding and cooperation of the natural gas industry. The SGR project is a field-based program using an integrated multidisciplinary approach that integrates geology, geophysics, engineering, and petrophysics. A major objective of this research project is to develop, test, and verify those technologies and methodologies that have near- to mid-term potential for maximizing recovery of gas from conventional reservoirs in known fields. Natural gas reservoirs in the Gulf Coast Basin are targeted as data-rich, field-based models for evaluating infield development. The SGR research program focuses on sandstone-dominated reservoirs in fluvial-deltaic plays within the onshore Gulf Coast Basin of Texas. The primary project research objectives are: To establish how depositional and diagenetic heterogeneities cause, even in reservoirs of conventional permeability, reservoir compartmentalization and hence incomplete recovery of natural gas. To document examples of reserve growth occurrence and potential from fluvial and deltaic sandstones of the Texas Gulf Coast Basin as a natural laboratory for developing concepts and testing applications. To demonstrate how the integration of geology, reservoir engineering, geophysics, and well log analysis/petrophysics leads to strategic recompletion and well placement opportunities for reserve growth in mature fields.

  13. Upwelling-driven reworking of a MTD's fine-grained plume: an example at the Cariaco Basin/Cariaco Gulf connection.

    Science.gov (United States)

    Aguilar, Iliana; Beck, Christian; Audemard, Franck; Crouzet, Christian; Sabatier, Pierre; Develle, Anne-Lise; Boussafir, Mohammed; Campos, Corina

    2016-04-01

    The Cariaco Basin is a 1400 m-deep and 90 km-wide pull-apart basin, in the south-eastern corner of the Caribbean Sea. To the East, it is connected to the Cariaco Gulf, a 60 km-long, 15 km-wide, and 90 m-deep appendix. Both are E-W elongated and developed upon the south-eastern transform boundary of the Caribbean Plate, an active limit here mainly represented by the El Pilar Fault. The Gulf of Cariaco entrance is a 55 m-deep, and 5 km-wide sill mainly controlled by the large Manzanares River delta, which western foreset slope is facing the Basin's eastern edge. Within this connection area, two particular sedimentary processes have been previously documented: 1) strong seasonal upwelling responsible for the transfer of deep particulate organic matter from the Basin into the Gulf; 2) the recent occurrence, in the Basin, of a fine-grained suspension related to a submarine landslide; this event was detected after the 1997 Cariaco earthquake (Thunell et al., 1999; Lorenzoni et al., 2012) and was related to a slope failure of the Manzanares delta western foreset. From short gravity cores retrieved in the Gulf, we analysed the last millennium of sedimentation (components, transport and settling processes) using classical proxies and physical properties. All parameters led to underline: - a permanent mixed provenance of particulate Organic Matter in the main part of the Gulf: i) in situ and ii) allochtonous; - the occurrence of coarse siliciclastic layers related to flooding from the southern edge of the Gulf; - the occurrence of one peculiar fine-grained siliciclastic layer with a widespread distribution, dated around 1850 AD; - an abrupt increase of open marine influence just after the above-mentioned layer. Concerning the "background" permanent sedimentation, these results confirm the importance of upwelling through the connection between the Gulf and the Basin (transfer of the "allochtonous" O.M.). For the fine-grained silicilastic "event", we could discard a

  14. Down Core Oxygen Isotopic Measurements Of Diatom δ18O From The Guaymas Basin, Gulf Of California

    Science.gov (United States)

    Menicucci, A. J.; Spero, H. J.; Thunell, R.

    2015-12-01

    The Guaymas Basin (GB), Gulf of California (27º53'N, 111º40'W ), is an evaporative basin, with sea surface temperatures (SST) varying between ~30oC (summer) and ~15oC (winter). Productivity is controlled mostly by seasonal upwelling starting in fall (early November) and extending into spring. We are currently analyzing δ18Odiatom from a boxcore (BC-43) using microfluorination (Menicucci, et al. 2013). This boxcore was previously analyzed for UK '37 alkenones and 210Pb activity (Goni, et al. 2001). Residual BC-43 material was sampled at ~2cm intervals. Samples were cleaned to isolate diatoms from other sediments, then equilibrated in water with δ18Owater = +85‰ for 70 hours at 21oC prior to vacuum dehydroxylation and microfluorination. The latter equilibration was done to account for fractionation between covalently bound O and OH- groups during vacuum dehydroxylation, preserving the original δ18Odiatom value. We present δ18Odiatom data from BC-43 samples covering 27cm, equivalent to >225 years of sediment accumulation. δ18O data are converted to temperature (T) based on an existing calibration (Leclerc and Labeyrie 1987). Our data suggest δ18Odiatom values record a T range of 22-18oC, corresponding to the mixed layer depth and the chlorophyll maximum during the fall bloom. These T values are offset from SST data by a mean of 5oC for the same sample intervals. However, δ18Odiatom values from the most recent samples suggest a ~2oC increase in diatom T relative to SST during the last 35 years. This subsurface warming may be due to decreased fall upwelling, increased mixed layer and chlorophyll maximum depths, and/or the timing of the peak diatom bloom. Such correlations are being investigated and the latest results will be presented. Goni, M. A., et al. (2001). Oceanographic considerations for the application of the alkenone-based paleotemperature U-37(K ') index in the Gulf of California. Geochimica Et Cosmochimica Acta 65: 545-557. Leclerc, A. J. and L

  15. Resource Assessment of the In-Place and Potentially Recoverable Deep Natural Gas Resource of the Onshore Interior Salt Basins, North Central and Northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini; Paul Aharon; Donald A. Goddard; Roger Barnaby

    2005-10-28

    The principal research effort for Year 2 of the project has been petroleum system characterization and modeling. Understanding the burial, thermal maturation, and hydrocarbon expulsion histories of the strata in the onshore interior salt basins of the North Central and Northeastern Gulf of Mexico areas is important in hydrocarbon resource assessment. The underburden and overburden rocks in these basins and subbasins are a product of their rift-related geohistory. Petroleum source rock analysis and initial thermal maturation and hydrocarbon expulsion modeling indicated that an effective regional petroleum source rock in the onshore interior salt basins and subbasins, the North Louisiana Salt Basin, Mississippi Interior Salt Basin, Manila Subbasin and Conecuh Subbasin, was Upper Jurassic Smackover lime mudstone. The initial modeling also indicated that hydrocarbon generation and expulsion were initiated in the Early Cretaceous and continued into the Tertiary in the North Louisiana Salt Basin and the Mississippi Interior Salt Basin and that hydrocarbon generation and expulsion were initiated in the Late Cretaceous and continued into the Tertiary in the Manila Subbasin and Conecuh Subbasin. Refined thermal maturation and hydrocarbon expulsion modeling and additional petroleum source rock analysis have confirmed that the major source rock in the onshore interior salt basins and subbasins is Upper Jurassic Smackover lime mudstone. Hydrocarbon generation and expulsion were initiated in the Early to Late Cretaceous and continued into the Tertiary.

  16. Bacterial sulfate reduction in hydrothermal sediments of the Guaymas Basin, Gulf of California, Mexico

    DEFF Research Database (Denmark)

    Weber, A.; Jørgensen, BB

    2002-01-01

    Depth distribution and temperature dependence of bacterial sulfate reduction were studied in hydrothermal surface sediments of the southern trough of the Guaymas Basin at 2000 m water depth. In situ temperatures ranged from 2.8 degreesC at the sediment surface to > 130degreesC at 30 cm depth in t...

  17. Reconstructing hypoxia of the southeastern Gulf of California over the last 18,000 years: sediments of Pescadero Basin

    Science.gov (United States)

    Choumiline, K.; Lyons, T.; Perez-Cruz, L. L.; Escorza-Reyes, M.; Bates, S.

    2014-12-01

    We present the first high-resolution multiproxy reconstruction of the past 18,000 years of oceanic redox variability in the southeastern Gulf of California (GC) and eastern Pacific. The variation in oxygen content prove to be a crucial regulator responsible for changes in biota distribution, water chemistry, physicochemical transformations of dissolved and particulate phases for trace elements in the water column, and formation of authigenic minerals, among other effects. The gravity core DIPAL-III T2 collected aboard the R/V "El Puma" (UNAM) from Pescadero Basin, located within the oxygen minimum zone (OMZ) of the southern GC, was thoroughly studied in terms of C, S, trace element and Fe speciation. After establishing the age-model of the marine sediments, the produced data revealed two clear episodes of peleoceanographic variability, associated with changes in hypoxia. The first period (18.0 - 11.6 cal kyr BP), represented by massive sediments, points to a time with an oxygenated water column and moderate productivity, elucidated by low Corg, high S and a relatively low redox sensitive trace element content (Mo and U). The second (11.6 cal kyr BP - present), easily perceived by a clear lamination pattern, indicates a suboxic/anoxic episode, evidenced by higher Corg, Mo and U, among others. A clear dramatic shift is distinctly observable between these periods for most of the redox-proxies. This shift is related to the changes in sea-level that immediately followed the Last Glacial Maximum, when the ice sheets began to melt. This transitioned Pescadero hydrochemistry from a shallow well-ventilated basin (prior to 11.6 cal kyr BP) to a deep OMZ system. When compared to renowned marine sedimentary records, such as Cariaco and Guaymas basins, some events became more eminent than others. In the particular case of the Younger Dryas (YD) stadial and Bolling Allerod (BA) interstadial, the Corg, S and some trace element patterns were similar among basins even from

  18. Snook (Centropomidae) and grouper (Serranidae) mariculture in the Gulf of Mexico and Caribbean Basin

    OpenAIRE

    Roberts Jr, D

    1989-01-01

    Centropomidae and Serranidae, sometimes collectively misnamed "sea basses", are suitable for aquaculture in pens, ponds, and raceways around the tropical and subtropical latitudes of the world. Western Atlantic Ocean species were recently considered for farming. South Florida, Mexico, Central and South America and the Antilles areas of the Caribbean Basin have extensive areas suitable for farming groupers and snook. Principal species of interest are the common snook (Centropomus undecimalis )...

  19. Relationship between salt diapirism and faulting in the central structural belt of the Dongying sag, Bohai Gulf basin, China

    Institute of Scientific and Technical Information of China (English)

    YU Jianguo; LI Sanzhong; WANG Jinduo; TIMOTHY M Kusky; WANG Xinhong; LU Shengqiang

    2005-01-01

    Many growth faults developed in the Dongying sag of the Jiyang depression of the Bohai Gulf basin, China. These normal growth faults consist of flower-like grabens in the hanging walls of the major faults, accompanied by reverse dragging. The central structural belt is an important structural unit in the Dongying sag, and is divided into a series of small blocks by these faults. These internal blocks can be classified into five structural classes, including parallel blocks, arc-shape blocks, plume-like blocks, ring-radial blocks,and splay blocks. It is shown that these complicated block classes and the "negative flower-like" fault associations in the central structural belt resulted from regional NNW-SSE extension accompanying local salt diapirism and related reverse dragging, rather than strike-slip faulting. On the basis of the diapirism strength, diapers in the central structural belt can be divided into lower salt ridges and pillows, and blind piercing structures. Diapirs are mainly composed of some salts with a little soft mudstone and gypsum. These structures began forming during deposition of the Sha 3 member and terminated during deposition of the Guangtao formation.

  20. Data collection for cooperative water resources modeling in the Lower Rio Grande Basin, Fort Quitman to the Gulf of Mexico.

    Energy Technology Data Exchange (ETDEWEB)

    Passell, Howard David; Pallachula, Kiran (GRAM, Inc., Albuquerque, NM); Tidwell, Vincent Carroll; Villalobos, Joshua (Texas A& M University); Piccinni, Giovanni (Texas A& M University); Brainard, James Robert; Gerik, Thomas (Texas A& M University); Morrison, Wendy (Texas A& M University); Serrat-Capdevila, Aleix (University of Arizona); Valdes, Juan (University of Arizona); Sheng, Zhuping (Texas A& M University); Lovato, Rene (Instituto Mexicano de Tecnologia del Agua); Guitron, Alberto (Instituto Mexicano de Tecnologia del Agua); Ennis, Martha Lee; Aparicio, Javier (Instituto Mexicano de Tecnologia del Agua); Newman, Gretchen Carr (GRAM, Inc., Albuquerque, NM); Michelsen, Ari M. (Texas A& M University)

    2004-10-01

    Water resource scarcity around the world is driving the need for the development of simulation models that can assist in water resources management. Transboundary water resources are receiving special attention because of the potential for conflict over scarce shared water resources. The Rio Grande/Rio Bravo along the U.S./Mexican border is an example of a scarce, transboundary water resource over which conflict has already begun. The data collection and modeling effort described in this report aims at developing methods for international collaboration, data collection, data integration and modeling for simulating geographically large and diverse international watersheds, with a special focus on the Rio Grande/Rio Bravo. This report describes the basin, and the data collected. This data collection effort was spatially aggregated across five reaches consisting of Fort Quitman to Presidio, the Rio Conchos, Presidio to Amistad Dam, Amistad Dam to Falcon Dam, and Falcon Dam to the Gulf of Mexico. This report represents a nine-month effort made in FY04, during which time the model was not completed.

  1. Sulfur, carbon, and oxygen isotope variations in submarine hydrothermal deposits of Guaymas Basin, Gulf of California, USA

    Science.gov (United States)

    Peter, J.M.; Shanks, Wayne C., III

    1992-01-01

    Sulfur, carbon, and oxygen isotope values were measured in sulfide, sulfate, and carbonate from hydrothermal chimney, spire, and mound samples in the southern trough of Guaymas Basin, Gulf of California, USA. ??34S values of sulfides range from -3.7 to 4.5%. and indicate that sulfur originated from several sources: 1. (1) dissolution of 0??? sulfide contained within basaltic rocks, 2. (2) thermal reduction of seawater sulfate during sediment alteration reactions in feeder zones to give sulfide with positive ??34S, and 3. (3) entrainment or leaching of isotopically light (negative-??34S) bacteriogenic sulfide from sediments underlying the deposits. ??34S of barite and anhydrite indicate sulfur derivation mainly from unfractionated seawater sulfate, although some samples show evidence of sulfate reduction and sulfide oxidation reactions during mixing within chimneys. Oxygen isotope temperatures calculated for chimney calcites are in reasonable agreement with measured vent fluid temperatures and fluid inclusion trapping temperatures. Hydrothermal fluids that formed calcite-rich chimneys in the southern trough of Guaymas Basin were enriched in 18O with respect to seawater by about 2.4??? due to isotopic exchange with sedimentary and/or basaltic rocks. Carbon isotope values of calcite range from -9.6 to -14.0??? ??34CpDB, indicating that carbon was derived in approximately equal quantities from the dissolution of marine carbonate minerals and the oxidation of organic matter during migration of hydrothermal fluid through the underlying sediment column. Statistically significant positive, linear correlations of ??34S, ??34C, and ??18O of sulfides and calcites with geographic location within the southern trough of Guaymas Basin are best explained by variations in water/rock ( w r) ratios or sediment reactivity within subsurface alteration zones. Low w r ratios and the leaching of detrital carbonates and bacteriogenic sulfides at the southern vent sites result in relatively

  2. Evidence of a Volcanic Rifted Margin: A Velocity Model for the Gulf of Mexico Basin Opening Seismic Refraction Project

    Science.gov (United States)

    Duncan, Mark; Van Avendonk, Harm; Christeson, Gail

    2013-04-01

    The Gulf of Mexico Basin Opening marine seismic refraction project (GUMBO) is a study of the lithological composition and structural evolution of the Gulf of Mexico (GoM) that uses Ocean Bottom Seismometer (OBS) data from four transects in the Northern GoM. Our analysis focuses specifically on line 4, the easternmost transect which extends over ~500 km from the continental shelf near Gainesville across the Florida Escarpment to the deep water GoM. Shear-wave first arrivals are picked from eleven out of the 39 OBS shot records in order to perform a tomographic inversion. The resulting shear-wave velocity model is used in conjunction with a previously constructed P-wave model to plot Vs as a function of Vp. We compare the Vp-Vs relationship with empirical velocities from the literature for the purpose of constraining lithological composition along GUMBO Line 4, and we make an interpretation of the structural evolution of the eastern GoM. The crust landward of the Florida Escarpment appears from our comparison with external data to be normal continental crust. Velocities plot within ~100 -200 m/s from compilations of seismic velocities (Vp = 6.2 - 7.0 km/sec; Vs = 3.8 - 4.0 km/sec) of felsic crystalline basement. Seaward of the escarpment, velocities in the oceanic crust are anomalously high (Vp = 6.5 - 7 km/sec; Vs = 4.0 - 4.6 km/sec). A possible explanation for this is that early-Jurassic basaltic sheet flows formed subaerially, reducing the vesicularity found in basalts that have cooled rapidly underwater. An increased magnesium and iron content could also account for these high velocities, and would suggest that the oceanic crust formed at higher mantle potential temperatures than previously thought. Geometrically, the transition from thick to thin crust near the Florida Escarpment on GUMBO line 4 is relatively narrow, which may be explained by rapid continental breakup with little stretching of continental crust. Alternatively, this margin may also have

  3. ASSESSING AND FORECASTING, BY PLAY, NATURAL GAS ULTIMATE RECOVERY GROWTH AND QUANTIFYING THE ROLE OF TECHNOLOGY ADVANCEMENTS IN THE TEXAS GULF COAST BASIN AND EAST TEXAS

    Energy Technology Data Exchange (ETDEWEB)

    William L. Fisher; Eugene M. Kim

    2000-12-01

    A detailed natural gas ultimate recovery growth (URG) analysis of the Texas Gulf Coast Basin and East Texas has been undertaken. The key to such analysis was determined to be the disaggregation of the resource base to the play level. A play is defined as a conceptual geologic unit having one or more reservoirs that can be genetically related on the basis of depositional origin of the reservoir, structural or trap style, source rocks and hydrocarbon generation, migration mechanism, seals for entrapment, and type of hydrocarbon produced. Plays are the geologically homogeneous subdivision of the universe of petroleum pools within a basin. Therefore, individual plays have unique geological features that can be used as a conceptual model that incorporates geologic processes and depositional environments to explain the distribution of petroleum. Play disaggregation revealed important URG trends for the major natural gas fields in the Texas Gulf Coast Basin and East Texas. Although significant growth and future potential were observed for the major fields, important URG trends were masked by total, aggregated analysis based on a broad geological province. When disaggregated by plays, significant growth and future potential were displayed for plays that were associated with relatively recently discovered fields, deeper reservoir depths, high structural complexities due to fault compartmentalization, reservoirs designated as tight gas/low-permeability, and high initial reservoir pressures. Continued technology applications and advancements are crucial in achieving URG potential in these plays.

  4. Development of the Cerro solo deposit and uranium favorability of the San Jorge Gulf Basin, province of Chubut

    International Nuclear Information System (INIS)

    In the future the uranium exploration activities of CNEA would tend to improve the knowledge of geology and uranium favorability; to perform prospection tasks, and research and development in exploration technologies, to contribute to be in a position to meet the requirements of the country in the long term. On the other hand, a strong growth of nuclear capacity is expected in the first two decades of the next century. Based on its promising grade, the Cerro Solo uranium ore deposit was selected in 1990 by the CNEA to carry out an assessment project. The intensive exploration level was accomplished, as follows: definition of general characteristics of the main orebodies; detailed geologic studies; estimation of resources with adequate data; and preliminary selection of mining-milling methods to estimate the potential profitability of the project. The deposit belongs to the sandstone type. The mineralized layers are distributed into the fluvial sandstones and conglomerates of the cretaceous Chubut Group, lying 50 to 130 m deep Resources of the deposit, with an average grade of 0.3% U, in tonnes of recoverable uranium at costs of up to $80/kg U, are: Reasonable Assured Resources (RAR): 800 t U, Estimated Additional Resources, Category I (EAR-I): 2100 t U. Follow-up drilling programmes are being performed at present in some of the target sites defined in the paleochannel that hosts the Cerro Solo deposit, in order to establish the hypothetical resources of the area. The sites were determined as a result of the exploration that CNEA conducted in the Pichinan uranium district. Recently a regional research project was formulated, for the detailed exploration in the San Jorge Gulf Basin, where the Chubut Group is distributed. 17 refs, 4 figs

  5. Glacial to Holocene terrigenous organic matter input to sediments from Orca Basin, Gulf of Mexico — A combined optical and biomarker approach

    OpenAIRE

    Meckler, A. N.; Schubert, C. J.; Hochuli, P. A.; Birgit Plessen; Birgel, D.; Flower, B. P.; K.-U. Hinrichs; Haug, G.H.

    2008-01-01

    In this study we assessed changes in the contribution of terrigenous organic matter (OM) to the Gulf of Mexico over the course of the last deglaciation (the last 25 kyr). To this end, we combined optical kerogen analyses with bulk sedimentary, biomarker, and compound-specific carbon isotope analyses. Samples were obtained from core MD02-2550 from Orca Basin (2249 m water depth at 26°56.77N, 91°20.74W) with temporal resolution ranging from multi-decadal to millennial-scale, depending on the pr...

  6. Resource Assessment of the In-Place and Potentially Recoverable Deep Natural Gas Resource of the Onshore Interior Salt Basins, North Central and Northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini; Donald A. Goddard

    2004-10-28

    The objectives of the study are: to perform resource assessment of the in-place deep (>15,000 ft) natural gas resource of the onshore interior salt basins of the North Central and Northeastern Gulf of Mexico areas through petroleum system identification, characterization and modeling and to use the petroleum system based resource assessment to estimate the volume of the in-place deep gas resource that is potentially recoverable and to identify those areas in the interior salt basins with high potential to recover commercial quantities of the deep gas resource. The principal research effort for Year 1 of the project is data compilation and petroleum system identification. The research focus for the first nine (9) months of Year 1 is on data compilation and for the remainder of the year the emphasis is on petroleum system identification.

  7. Seismic reflection-based evidence of a transfer zone between the Wagner and Consag basins: implications for defining the structural geometry of the northern Gulf of California

    Science.gov (United States)

    González-Escobar, Mario; Suárez-Vidal, Francisco; Hernández-Pérez, José Antonio; Martín-Barajas, Arturo

    2010-12-01

    This study examines the structural characteristics of the northern Gulf of California by processing and interpreting ca. 415 km of two-dimensional multi-channel seismic reflection lines (data property of Petróleos Mexicanos PEMEX) collected in the vicinity of the border between the Wagner and Consag basins. The two basins appear to be a link between the Delfín Superior Basin to the south, and the Cerro Prieto Basin to the north in the Mexicali-Imperial Valley along the Pacific-North America plate boundary. The seismic data are consistent with existing knowledge of four main structures (master faults) in the region, i.e., the Percebo, Santa María, Consag Sur, and Wagner Sur faults. The Wagner and Consag basins are delimited to the east by the Wagner Sur Fault, and to the west by the Consag Sur Fault. The Percebo Fault borders the western margin of the modern Wagner Basin depocenter, and is oriented N10°W, dipping (on average) ˜40° to the northeast. The trace of the Santa María Fault located in the Wagner Basin strikes N19°W, dipping ˜40° to the west. The Consag Sur Fault is oriented N14°W, and dips ˜42° to the east over a distance of 21 km. To the east of the study area, the Wagner Sur Fault almost parallels the Consag Sur Fault over a distance of ˜86 km, and is oriented N10°W with an average dip of 59° to the east. Moreover, the data provide new evidence that the Wagner Fault is discontinuous between the two basins, and that its structure is more complex than previously reported. A structural high separates the northern Consag Basin from the southern Wagner Basin, comprising several secondary faults oriented NE oblique to the main faults of N-S direction. These could represent a zone of accommodation, or transfer zone, where extension could be transferred from the Wagner to the Consag Basin, or vice versa. This area shows no acoustic basement and/or intrusive body, which is consistent with existing gravimetric and magnetic data for the region.

  8. "Who's afraid of Virginia Woolf?" : Edward Albee y su influencia en el teatro de Alfonso Paso

    OpenAIRE

    Espejo Romero, Ramón

    1998-01-01

    Edward Albee's Who's Afraid of Virginia Woolf? (1962) is, without any doubt, one of the most significant American dramas of the 1960s. The fame of Albee's highly controversial play soon reached Spain, for a Spanish version of it was successfully presented in Madrid in 1966. An unexpected consequence of the play's sudden popularity was the influence it exerted on the dramatic works of Spanish playwright Alfonso Paso. This paper studies the way in which Who's Afraid of Virginia Woolf?'s Spanish...

  9. Early Diagenetic Effects on Magnetic Properties in Laminated Sediments from the Southern Gulf of California

    Science.gov (United States)

    Perez-Cruz, L. L.; Fucugauchi, J. U.

    2015-12-01

    Effects of early diagenesis on the magnetic mineralogy in marine sediments have long been investigated, including oxidation/reduction reactions, magnetic dilution, formation of iron sulfides and oxides, magnetization acquisition mechanisms and reliability of paleomagnetic record. In this study, we analyze the mineral magnetic properties and downcore magnetite contents on Late Holocene sediments from Alfonso Basin, Gulf of California. Volcanic-derived terrigenous and biogenic input represents major sediment sources, with low-oxygen environments allowing preservation of finely laminated sequences. Susceptibility logs show high values at the top sediments and small amplitude low frequency fluctuations downcore. Magnetic hysteresis loops indicate low coercivity saturation characteristic of magnetites and low-Ti titanomagnetites, with varying paramagnetic contributions. Intensity of natural remanent magnetization, saturation isothermal magnetization and coercivity parameters show similar patterns with depth. In particular, the susceptibility log shows magnetic enhancement in the upper sediments of up to 4 times the values along the core. Below 40 cm depth the exponential decay relates to diagenetic changes and magnetite authigenesis associated with organic matter oxidative decomposition during dewatering and compaction occurring above the iron reduction zone. Results support presence of recent and old dissolution fronts resulting from preservation of enriched PSD/MD magnetite in between the dissolution fronts. Oxidation/reduction conditions in turn relate to climatic and water/sediment interface factors that control dissolution processes, which occur in sub-oxic to anoxic conditions.

  10. Recent Advances in Modeling Phosphorus and Nitrogen Delivery to the Gulf of Mexico and Implications for Managing Nutrients n the Mississippi River Basin

    Science.gov (United States)

    Alexander, R. B.; Smith, R. A.; Schwarz, G. E.; Boyer, E. W.; Nolan, J. V.; Brakebill, J. W.

    2008-12-01

    Although the increased availability of reactive nutrients in past decades has benefited society via food and energy production, the corresponding rise in nutrient loadings to aquatic ecosystems is of particular concern, especially in many estuaries globally where increased nutrient loads have contributed to eutrophic conditions. In the United States, elevated riverine nutrients have contributed to stressed trophic conditions in a majority of estuaries, including the shallow coastal waters of the Louisiana shelf in the northern Gulf of Mexico, where both nitrogen and phosphorus loadings are recognized as contributing to seasonal hypoxic conditions. Advances in geospatial modeling of nitrogen and phosphorus sources and transport in the Mississippi and Atchafalaya River Basins (MARB), as reported in a recent U.S. Geological Survey (USGS) study, provide important information to support improved assessments and management of nutrient loadings to the northern Gulf of Mexico. We summarize the findings of this study and discuss the implications for managing nutrient sources in the MARB. The study reveals important differences in the sources and aquatic transport of nitrogen and phosphorus that affect delivery to the Gulf. Although agricultural sources contribute a majority of the delivered nutrients to the Gulf, corn and soybean cultivation is the largest contributor of nitrogen whereas phosphorus originates primarily from animal manure on pasture and rangelands. Atmospheric deposition is the second leading source of nitrogen, with urban sources contributing relatively small quantities of both nutrients. Furthermore, we find that both nitrogen and phosphorus delivery to the Gulf is controlled by hydrological and biogeochemical processes (e.g., water travel time, denitrification, storage) that scale with stream size, although phosphorus also displays large local- and regional-scale differences in delivery caused by reservoir trapping. The importance of these processes

  11. RESOURCE ASSESSMENT OF THE IN-PLACE AND POTENTIALLY RECOVERABLE DEEP NATURAL GAS RESOURCE OF THE ONSHORE INTERIOR SALT BASINS, NORTH CENTRAL AND NORTHEASTERN GULF OF MEXICO

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini

    2004-04-16

    The University of Alabama and Louisiana State University have undertaken a cooperative 3-year, advanced subsurface methodology resource assessment project, involving petroleum system identification, characterization and modeling, to facilitate exploration for a potential major source of natural gas that is deeply buried (below 15,000 feet) in the onshore interior salt basins of the North Central and Northeastern Gulf of Mexico areas. The project is designed to assist in the formulation of advanced exploration strategies for funding and maximizing the recovery from deep natural gas domestic resources at reduced costs and risks and with minimum impact. The results of the project should serve to enhance exploration efforts by domestic companies in their search for new petroleum resources, especially those deeply buried (below 15,000 feet) natural gas resources, and should support the domestic industry's endeavor to provide an increase in reliable and affordable supplies of fossil fuels. The principal research effort for Year 1 of the project is data compilation and petroleum system identification. The research focus for the first nine (9) months of Year 1 is on data compilation and for the remainder of the year the emphasis is on petroleum system identification. The objectives of the study are: to perform resource assessment of the in-place deep (>15,000 ft) natural gas resource of the onshore interior salt basins of the North Central and Northeastern Gulf of Mexico areas through petroleum system identification, characterization and modeling and to use the petroleum system based resource assessment to estimate the volume of the in-place deep gas resource that is potentially recoverable and to identify those areas in the interior salt basins with high potential to recover commercial quantities of the deep gas resource. The project objectives will be achieved through a 3-year effort. First, emphasis is on petroleum system identification and characterization in the

  12. Origin and early development of the Gulf of Mexico Basin based on 15-second record seismic in the Louisiana Shelf and Upper Slope

    Energy Technology Data Exchange (ETDEWEB)

    Hall, D.J. [Excalibur Interpretation Co., Houston, TX (United States)

    1996-09-01

    A 4x4 mile grid of new 15-second record seismic data covering the entire Louisiana shelf and upper slope reveals new insights into the deep structure of the Gulf of Mexico Basin. Noteworthy is the absence of evidence for major horst and graben basement faulting predicted in some models for the early Gulf under the shelf. Instead, the basement appears generally smooth, with a reasonably conformable early section 1 to 1.5 seconds thick immediately overlying it. This suggests either that the basement was formed as lower plate continental crust (in a simple shear detachment fault scenario, below the brittle-ductile crustal transition) or as oceanic crust similar to that observed under autochthonous salt in the Perdido fold belt. If the latter is correct, the edge of oceanic crust needed to reconstruct the sea-floor spreading history may nearly coincide with the current northern limit of the sub-salt hydrocarbon play, possibly because the play location depends on 3-4 km thick salt originally deposited in the area under the southern shelf. The southern limit of thick LouAnn salt is related to depositional factors (evaporation, oceanic circulation, etc.) rather than to underlying crustal type. An unresolved question is the nature of the section overlying the smooth basement event. Both deepwater Lower Cretaceous (chalks, marts ?) and Eagle Mills deepwater equivalents (shales) are plausible interpretations.

  13. Dinoflagellate cysts as indicators of millennial scale climatic and oceanographic variability in Guaymas Basin, Gulf of California (Mexico) during the Late Quaternary

    Science.gov (United States)

    Price, Andrea M.; Mertens, Kenneth N.; Pospelova, *Vera; Pedersen, Thomas F.; Ganeshram, Raja S.

    2015-04-01

    A high-resolution record of organic-walled dinoflagellate cyst production in Guaymas Basin, Gulf of California (Mexico) reveals a complex paleoceanographic history over the last ~40 ka. Guaymas Basin is an excellent location to perform high resolution studies of changes in Late Quaternary climate and paleo-productivity because it is characterized by high primary productivity, high sedimentation rates, and low oxygen bottom waters. These factors contribute to the deposition and preservation of laminated sediments throughout large portions of core MD02-2515. This is one of the first studies in the Northeast Pacific to document dinoflagellate cyst production at a centennial to millennial scale throughout the Late Quaternary. Based on the cyst assemblages three major dinoflagellate cyst zones were established, and roughly correspond to Marine Isotope Stages 1 to 3. The most dominant dinoflagellate cyst taxa found throughout the core were Brigantedinium spp. and Operculodinium centrocarpum. Dansgaard-Oeschger event 8 is observed in the dinoflagellate cyst record, and is characterized by an increase in warm water taxa such as Spiniferites pachydermus. Other intervals of interest are the Younger Dryas where cooler sea-surface conditions are not recorded, and the Holocene which is characterized by the consistent presence of warm water species Stelladinium reidii, Tuberculodinidum vancampoae, Bitectatodinium spongium and an increase in Quinquecuspis concreta. Changes in cyst assemblages, concentrations and species diversity, along with geochemical data reflect major orbital to millennial-scale climatic and oceanographic changes. Keywords: Dansgaard-Oeschger events; dinoflagellate cyst; Gulf of California; late Quaternary climate change; upwelling; Younger Dryas.

  14. Gulf Coast Geology (GCG) Online

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — A large percentage of the present and future energy resources of the United States reside in the Gulf of Mexico Basin, one of the major hydrocarbon producing areas...

  15. Modelo de servicio Biblioteca Alfonso Borrero Cabal, S.J. de la Pontificia Universidad Javeriana

    OpenAIRE

    2013-01-01

    El trabajo tiene como propósito demostrar la importancia que tiene el servicio en toda organización, en este caso aplicado a la Biblioteca Alfonso Borrero Cabal S,J, de la Pontificia Universidad Javeriana. La definición del modelo de servicio se inició con un diagnóstico para verificar como se está prestando el servicio en la actualidad, confirmar los procesos existentes y generar las recomendaciones pertinentes. A partir de la información obtenida, se definió el modelo para la unidad de info...

  16. Does a strong pycnocline impact organic-matter preservation and accumulation in an anoxic setting? The case of the Orca Basin, Gulf of Mexico

    Science.gov (United States)

    Tribovillard, Nicolas; Bout-Roumazeilles, Viviane; Sionneau, Thomas; Serrano, Jean Carlos Montero; Riboulleau, Armelle; Baudin, François

    2009-01-01

    The Orca Basin (an intraslope depression located in the Gulf of Mexico) collects sedimentary particles of terrestrial origin (clastic and organic particles mainly supplied by the Mississippi River) and of marine origin (biogenic productivity). The basin is partly filled with dense brines leached from salt diapirs cropping out on the sea floor, and is permanently stratified. A strong pycnocline induces anoxic bottom conditions, expectedly favorable to organic matter (OM) preservation. Here, we report on OM in the upper 750 cm below sea floor of Core MD02-2552 (Holocene). The organic content is dominated by marine-derived amorphous OM. The organic assemblage is unexpectedly degraded to some extent, which may be accounted for by a relatively long residence time of organic particles at the halocline-pycnocline at ˜2240 m. Thus the organic particles are temporarily trapped and kept in contact with the dissolved oxygen-rich overlying water mass. Lastly, the land-derived organic fraction shows co-variations with the land-derived clay mineral supply.

  17. Energy flux and hydrogeology of thermal anomalies in the Gulf of Mexico Basin -- South Texas example. Progress report, [1 September 1993--28 February 1994

    Energy Technology Data Exchange (ETDEWEB)

    Sharp, J.M. Jr.

    1994-03-01

    This report covers the period from 1 September 1993 through 28 February 1994. The last Technical Progress Report was submitted in September 1993. In this period, we have focused our efforts on the following activities (a more detailed description of each effort is (1) Finalizing collection of radiogenic heat production data; (2) Evaluating petrographic controls on thermal conductivity; (3) Modeling one-dimensional heat conduction with sources; (4) Completing base geologic cross-section; (5) Acquiring pressure data to augment data base; (6).Putting map and well data into digital format for analysis; (7) Analyzing salinity, temperate and fluid potential data for propensity of free convection; (8) Finalizing preliminary investigation into depressurization of reservoirs; (9) Preparing presentations for AAPG meeting in Denver; (10) Presenting results at the Geological Society of America Meeting in Boston (October 1993); (11) Collaborating with project members of the DOE funded Global Basins Research Network who are working on a project in the Eugene Island Block, offshore Louisiana; and (12) Collaborating with others working on research in the Gulf of Mexico Basin in our Department and with CSIRO scientists in Adelaide, Australia.

  18. Modified Gulf of California model for South Georgia,north Scotia Ridge, and implications for the Rocas Verdes back-arc basin, southern Andes

    Science.gov (United States)

    Alabaster, T.; Storey, B. C.

    1990-06-01

    New field mapping and an integrated trace element and Nd isotopic study have been undertaken on the Jurassic-Cretaceous Larsen Harbour Complex on the island of South Georgia, recognized as a displaced part of the southern Andes ensialic, autochthonous Rocas Verdes marginal basin. Five basalt groups (Groups I-V) are identified from trace element data; initial Nd isotopic compositions suggest that they are derived from only two sources. Magmas produced during early stages of continental lithospheric attenuation (Groups I-III) were derived by varying degrees of partial melting and fractional crystallization from a large ion lithophile element (LILE)-enriched, low-ɛNd mantle source relative to normal (N)-type mid-ocean ridge basalt (MORB). Magmas produced during later stages of rifting (Groups IV and V) were, however, derived from a high-ɛNd asthenospheric mantle source similar to N-type MORB, unaffected by earlier LILE enrichment. Our data do not concur with previous suggestions that the Larsen Harbour Complex and, by implication, the Rocas Verdes formed in a supra-subduction-zone setting. On the basis of geologic and geochemical evidence, we favor basin formation along an oblique-slip margin akin to that of the Gulf of California.

  19. Historia de los MSS BH 133 y 128 de Alfonso de Palencia

    Directory of Open Access Journals (Sweden)

    Durán Barceló, Javier

    2012-07-01

    Full Text Available El investigador que inspeccione los volúmenes UCM BH MSS 133 y 128 de Alfonso de Palencia encontrará un buen número de marcas y cotas librarias acumuladas a lo largo de su historia. Como veremos en este trabajo, estas signaturas tienen su correspondencia en los inventarios y catálogos de la biblioteca del Colegio de San Ildefonso desde 1720, 1745, 1800 y 1878. Además, la historia de estos manuscritos se puede rastrear hasta la fundación del Colegio mediante un examen analítico de los primitivos inventarios de la librería ildefonsina incluso más allá del año 1517.The researcher who inspects volumes UCM BH MSS 133 and 128 of Alfonso de Palencia will encounter a great variety of old call numbers and librarian marks accumulated throughout their history. As we will find out in this paper, these call numbers have also a parallel existence in the inventories and catalogues of the Library of the Colegio de San Ildefonso produced since 1720, 1745, 1800 y 1878. But the history of these manuscripts can be also traced back to the foundation of the College, as it is demonstrated by an analytical examination of the earlier Library inventories as far as 1517 and beyond.

  20. La China gótica de Alfonso Hernández Catá

    Directory of Open Access Journals (Sweden)

    Sandra Casanova-Vizcaíno

    2014-01-01

    Full Text Available Este artículo analiza dos cuentos del escritor cubano Alfonso Hernández Catá (1885-1940, “Los chinos” (1924 y “El gato” (1933, cuyos personajes asiáticos son descritos como seres grotescos y monstruosos tal como y ocurre en el género gótico. Esta monstruosidad de los chinos, además, se presenta como una enfermedad contagiosa que amenaza con contagiar y desestabilizar los límites entre la vida y la muerte, la cordura y la locura, la familiaridad y la extrañeza, Occidente y Oriente. This article analyzes two short stories by Cuban writer Alfonso Hernández Catá (1885-1940: “Los chinos” (1924 and “El gato” (1933. In these texts, Asian characters are described as grotesque and monstrous beings like the ones found in the Gothic genre. Moreover, this monstrosity is depicted as a contagious disease that threatens to infect and destabilize the boundaries between life and death, sanity and insanity, the familiar and the unknown, the West and the East.

  1. Rock magnetic properties of a holocene laminated sequence from the Gulf of California

    International Nuclear Information System (INIS)

    Complete text of publication follows. Results of a rock magnetic study of laminated sediments from the Alfonso Basin, Bay of La Paz are used to investigate sediment sources and depositional environment in the southern Gulf of California during the Holocene. AMS radiocarbon dating on benthic foram shells provides stratigraphic control, with age for the core bottom sediments of 7597-7831 cal. yr B.P. Magnetic signal is dominated by fine-grained titanomagnetites, derived from the silicic volcanic units surrounding the Bay of La Paz. Magnetic mineralogy is relatively homogenous as seen in bulk magnetic properties of low-field susceptibility, remanent intensity and coercivity. Magnetic hysteresis loops show strong variable paramagnetic components; after paramagnetic correction loops show saturation at low fields and high saturation magnetization values. Plots of hysteresis parameter ratios for domain state show that samples group in the pseudo-single domain field, with mixtures of single and multi-domain particles. Magnetic susceptibility logs show relatively high frequency dependence factors, particularly for the Middle Holocene, suggesting increased contribution of fine-grained superparamagnetic minerals related to eolian deposition. Magnetic susceptibility exhibits an apparent cyclicity of roughly 1200-1500 yr. Paramagnetic slope correction parameter shows higher values between 30 cm and 40 cm depth, with an apparent cyclic variation along the core. The well-preserved laminated sequence indicates predominant anoxic conditions in the basin floor. Depositional environment had a dominant supply of pluvial detrital sediments and eolian fine-grained dust composed of siliciclastic volcanically-derived material with less abundant biogenic input.

  2. Resource Assessment of the In-Place and Potentially Recoverable Deep Natural Gas Resource of the Onshore Interior Salt Basins, North Central and Northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Ernest A. Mancini

    2006-09-30

    The objectives of the study were: (1) to perform resource assessment of the thermogenic gas resources in deeply buried (>15,000 ft) natural gas reservoirs of the onshore interior salt basins of the north central and northeastern Gulf of Mexico areas through petroleum system identification, characterization and modeling; and (2) to use the petroleum system based resource assessment to estimate the volume of the deep thermogenic gas resource that is available for potential recovery and to identify those areas in the interior salt basins with high potential for this thermogenic gas resource. Petroleum source rock analysis and petroleum system characterization and modeling, including thermal maturation and hydrocarbon expulsion modeling, have shown that the Upper Jurassic Smackover Formation served as the regional petroleum source rock in the North Louisiana Salt Basin, Mississippi Interior Salt Basin, Manila Subbasin and Conecuh Subbasin. Thus, the estimates of the total hydrocarbons, oil, and gas generated and expelled are based on the assumption that the Smackover Formation is the main petroleum source rock in these basins and subbasins. The estimate of the total hydrocarbons generated for the North Louisiana Salt Basin in this study using a petroleum system approach compares favorably with the total volume of hydrocarbons generated published by Zimmermann (1999). In this study, the estimate is 2,870 billion barrels of total hydrocarbons generated using the method of Schmoker (1994), and the estimate is 2,640 billion barrels of total hydrocarbons generated using the Platte River software application. The estimate of Zimmermann (1999) is 2,000 to 2,500 billion barrels of total hydrocarbons generated. The estimate of gas generated for this basin is 6,400 TCF using the Platte River software application, and 12,800 TCF using the method of Schmoker (1994). Barnaby (2006) estimated that the total gas volume generated for this basin ranges from 4,000 to 8,000 TCF. Seventy

  3. A review on tectonic record of strain buildup and stress release across the Andean forearc along the Gulf of Guayaquil-Tumbes basin (GGTB) near Ecuador-Peru border

    OpenAIRE

    2013-01-01

    Gravimetric and geologic data show that the reactivation of the Neogene Interandean depression and/or the ~75 - 65 Ma ophiolite suture into the modern dynamic of the Andes controlled the Gulf of Guayaquil Tumbes basin (GGTB) location and evolution during the past 1.8 - 1.6 Myr at least. Depending on whether the remobilization occurred along the in- terandean depression or the ophiolite suture, the GGTB evolved trough pure or simple shear mechanisms, respectively. Because the GGTB exhibits an ...

  4. Depositional environment of Brushy Basin Member, Morrison Formation, in Gulf Mariano Lake mine, McKinley County

    International Nuclear Information System (INIS)

    The Mariano Lake mine, McKinley County, New Mexico, is developed in the lower portion of the Brushy Basin Member of the Morrison Formation (Upper Jurassic). The sandstones typically are arkosic to subarkosic, moderately to poorly sorted, medium to coarse grained, subrounded, carbonaceous, and silica cemented. Early emplacement of uranium minerals occurred along geochemical boundaries in a roll-front geometry. In the area of the Mariano mine, the Brushy Basin member was deposited as a series of stacked, lenticular-shaped sand bodies interfingering with bentonitic mudstones. Petrologic and sedimentologic data allow the interval to be divided into four depositional facies. These facies represent in-channel and flood-basin deposits of a braided-stream complex with characteristics of the present-day Platte River and Bijou Creek

  5. Continental breakup and the dynamics of rifting in back-arc basins: The Gulf of Lion margin

    Science.gov (United States)

    Jolivet, Laurent; Gorini, Christian; Smit, Jeroen; Leroy, Sylvie

    2015-04-01

    Deep seismic profiles and subsidence history of the Gulf of Lion margin reveal an intense stretching of the distal margin and strong postrift subsidence, despite weak extension of the onshore and shallow offshore portions of the margin. We revisit this evolution from the geological interpretation of an unpublished multichannel seismic profile and other published geophysical data. We show that an 80 km wide domain of thin lower continental crust, the "Gulf of Lion metamorphic core complex," is present in the ocean-continent transition zone and exhumed mantle makes the transition with oceanic crust. The exhumed lower continental crust is bounded upward and downward by shallow north dipping detachments. The presence of exhumed lower crust in the deep margin explains the discrepancy between the amount of extension deduced from normal faults in the upper crust and total extension. We discuss the mechanism responsible for exhumation and present two scenarios: the first one involving a simple coupling between mantle extension due to slab retreat and crustal extension and the second one involving extraction of the lower crust and mantle from below the margin by the southeastward flow of hot asthenosphere in the back-arc region during slab rollback. In both scenarios, the combination of Eocene crustal thickening related to the Pyrenees, the nearby volcanic arc, and a shallow lithosphere-asthenosphere boundary weakened the upper mantle and lower crust enough to make them flow southeastward. The overall hot geodynamic environment also explains the subaerial conditions during most of the rifting stage and the delayed subsidence after breakup.

  6. Adjustment of the basin-scale circulation at 26° N to variations in Gulf Stream, deep western boundary current and Ekman transports as observed by the Rapid array

    Directory of Open Access Journals (Sweden)

    S. A. Cunningham

    2009-04-01

    Full Text Available The Rapid instrument array across the Atlantic Ocean along 26° N provides unprecedented monitoring of the basin-scale circulation. A unique feature of the Rapid array is the combination of full-depth moorings with instruments measuring temperature, salinity, pressure time series at many depths with co-located bottom pressure measurements so that dynamic pressure can be measured from surface to bottom. Bottom pressure measurements show a zonally uniform rise (and fall of bottom pressure of 0.015 dbar on a 5 to 10 day time scale, suggesting that the Atlantic basin is filling and draining on a short time scale. After removing the zonally uniform bottom pressure fluctuations, bottom pressure variations at 4000 m depth against the western boundary compensate instantaneously for baroclinic fluctuations in the strength and structure of the deep western boundary current so there is no basin-scale mass imbalance resulting from variations in the deep western boundary current. After removing the mass compensating bottom pressure, residual bottom pressure fluctuations at the western boundary just east of the Bahamas balance variations in Gulf Stream transport. Again the compensation appears to be especially confined close to the western boundary. Thus, fluctuations in either Gulf Stream or deep western boundary current transports are compensated in a depth independent (barotropic manner very close to the continental slope off the Bahamas. In contrast, compensation for variations in wind-driven surface Ekman transport appears to involve fluctuations in both western basin and eastern basin bottom pressures, though the bottom pressure difference fluctuations appear to be a factor of 3 too large, perhaps due to an inability to resolve small bottom pressure fluctuations after removal of larger zonal average, baroclinic, and Gulf Stream pressure components. For 4 tall moorings where time series dynamic height (geostrophic pressure profiles can be estimated from

  7. Late Quaternary climatic and oceanographic changes in the Northeast Pacific as recorded by dinoflagellate cysts from Guaymas Basin, Gulf of California (Mexico)

    Science.gov (United States)

    Price, Andrea M.; Mertens, Kenneth N.; Pospelova, Vera; Pedersen, Thomas F.; Ganeshram, Raja S.

    2013-01-01

    A high-resolution record of organic-walled dinoflagellate cyst production in Guaymas Basin, Gulf of California (Mexico) reveals a complex paleoceanographic history over the last ~40 ka. Guaymas Basin is an excellent location to perform high resolution studies of changes in late Quaternary climate and paleo-productivity because it is characterized by high primary productivity, high sedimentation rates, and low oxygen bottom waters. These factors contribute to the deposition and preservation of laminated sediments throughout large portions of the core MD02-2515. In this study, we document dinoflagellate cyst production at a centennial to millennial scale throughout the late Quaternary. Based on the cyst assemblages, three dinoflagellate cyst zones were established and roughly correspond to Marine Isotope Stages (MISs) 1 to 3. MISs 1 and 3 are dominated by cysts of heterotrophic dinoflagellates, whereas MIS 2 is characterized by enhanced variability and a greater proportion of cysts produced by autotrophic taxa. The most dominant dinoflagellate cyst taxa found throughout the core were Brigantedinium spp. and Operculodinium centrocarpum. Dansgaard-Oeschger event 8 is observed in the dinoflagellate cyst record where it is characterized by an increase in warm taxa, such as Spiniferites pachydermus. Other intervals of interest are the Younger Dryas where warmer conditions are recorded and the Holocene which is characterized by the consistent presence of tropical species Stelladinium reidii, Tuberculodinidum vancampoae, Bitectatodinium spongium, and an increase in Quinquecuspis concreta. Changes in cyst assemblages, concentrations, and species diversity, along with geochemical data reflect major orbital to millennial-scale climatic and oceanographic changes.

  8. Alfonso Pérez-Agote y el oficio de sociólogo

    Directory of Open Access Journals (Sweden)

    Daniel Muriel

    2015-11-01

    Full Text Available En este artículo reflexiono sobre los fundamentos del oficio de sociólogo a partir de un axioma extraído de los preceptos teóricos de Alfonso Pérez-Agote, por el que la labor esencial del científico social descansa en aproximarse a las representaciones sociales que hacen los actores de la realidad en la que viven sin definirla de antemano. Este principio es puesto bajo la lupa crítica de ciertas corrientes contemporáneas posestructuralistas y matizado en consecuencia, sin renunciar, por ello, a su validez como fundamento que ha de regir el oficio sociológico.

  9. La doctrina sobre el poder del príncipe en Alfonso Hojeda de Mendoza

    Directory of Open Access Journals (Sweden)

    Salustiano de DIOS

    2009-12-01

    Full Text Available RESUMEN: Alfonso Hojeda fue un notable canonista sevillano que en 1576 publicó en Venecia un libro acerca de los beneficios eclesiásticos. La obra se divide en dos partes: la primera está dedicada a argumentar en contra de la pluralidad de beneficios en una misma persona, de acuerdo con los decretos tridentinos de reforma, mientras la segunda trata en cambio de la compatibilidad de beneficios mediante dispensa papal. Los propios términos en que se manifiestan las dos partes ya están indicando las contradicciones en que ha de moverse el autor, difíciles de salvar. La doctrina de la causa es, además de la distinción entre órdenes normativos, la principal herramienta conciliatoria para Hojeda. El papa está desligado del derecho positivo o humano, pues de otro modo no podría dispensar, o privilegiar, mas sólo puede hacerlo con justa causa.ABSTRACT: Alfonso Hojeda de Mendoza was an outstanding canonist that in 1576 published a book in Venice on the eclesiástica benefits. The book is divided into two parts: the first one is devoted to argue against the plurality of benefits in the same person, according to Trento's decrees, while the second one deals, however, with the compatibility of benefits by the Pope's dispense. The own terms in which both parts are expressed reveal the contradictions, in which the author must move, always difficult to avoid. The doctrine of the cause, as well as the distinction among normative orders, is the main conciliatory tool for Hojeda. The Pope is unlinked to human or positive right, otherwise he could not dispense or privilege, however he can only do it for a just cause.

  10. Garra mondica, a new species from the Mond River drainage with remarks on the genus Garra from the Persian Gulf basin in Iran (Teleostei: Cyprinidae).

    Science.gov (United States)

    Sayyadzadeh, Golnaz; Esmaeili, Hamid Reza; Freyhof, Jörg

    2015-01-01

    Garra mondica, new species, from the Mond River drainage in Iran is distinguished from its congeners by having 7½ branched dorsal-fin rays; the breast, belly and back in front of the dorsal-fin origin naked and 9+8 branched caudal-fin rays. Garra mondica is also distinguished from all other congeners in the Persian Gulf basin, except an unidentified species from the Kol River, by having two fixed, diagnostic nucleotide substitutions in the mtDNA COI barcode region. The identity of G. gymnothorax, a nominal species from the Karun River drainage, and G. crenulata, a nominal species from Central Iran, are discussed. Garra populations examined from the Karun have a unique mtDNA COI barcode sequence, but their diagnostic characters are not consistent with the description and syntypes of G. gymnothorax. G. crenulata is considered as a synonym of G. rufa. Two populations of Garra from the Kol River have a sequence of the COI barcode region very similar to G. mondica, but cannot be identified as G. mondica and their identity cannot be resolved here. PMID:26624737

  11. Texto e imagen en España de sol a sol de Alfonso Armada

    Directory of Open Access Journals (Sweden)

    Champeau, Geneviève

    2011-06-01

    Full Text Available España de sol a sol (2001 by Alfonso Armada gives an example of the development of the «travel narrative» genre in Spain today. Faced with the «end of travel» (Marc Augé, he proposes a renovation of the perception of the familiar by travelling across Spain and Portugal and by substituting «endotic» (Georges Pérec for exotic.The poetics in the narrative differs greatly from that by travelling writers of «social realism», in the Spain of the sixties. Interpretation replaces information, the poetic image prevails over the referential function of language, and polysemy, omnipresent intertexuality and metatextuality play an important part. The change also affects the links between text and image, which are now more complementary than redundant. Playing with stereotypes, the photography actively contributes to establishing argumentative strategies meant to make the reader-viewer adhere to the message, all while affirming itself as an autonomous aesthetic experience.España de sol a sol (2001 de Alfonso Armada proporciona una muestra de la evolución del género del «libro de viajes» en la España contemporánea. Ante la imposibilidad del viaje (Marc Augé, propone renovar la percepción de lo familiar recorriendo el espacio nacional y sustituyendo el «endotismo» (Georges Pérec al exotismo. La poética del viaje que propone el relato difiere profundamente de la de los escritores viajeros del «realismo social», en la España de los años sesenta, anteponiendo la interpretación a la información, la imagen poética a la función referencial del lenguaje, cultivando la polisemia, una intertextualidad masiva y una reflexión metatextual. Distintos son también los vínculos que se establecen entre texto e imagen, de complementariedad más que de redundancia. La fotografía participa activamente, por la reelaboración de tópicos, del dispositivo argumentativo destinado a favorecer la adhesión del lector-espectador al mensaje y se afirma

  12. Microbial mat records in siliciclastic rocks: Examples from Four Indian Proterozoic basins and their modern equivalents in Gulf of Cambay

    Science.gov (United States)

    Sarkar, Subir; Banerjee, Santanu; Samanta, Pradip; Chakraborty, Nivedita; Chakraborty, Partha Pratim; Mukhopadhyay, Soumik; Singh, Arvind K.

    2014-09-01

    Microbial mat-related structures (MRS) in siliciclastics have been investigated from four Proterozic formations in India, namely the Marwar Supergroup, the Vindhyan Supergroup, the Chhatisgarh Supergroup and the Khariar Group for their spectral variations, genetic aspects, palaeo-environmental significance and influence on sequence stratigraphic architecture. The maximum diversification of MRS has been experienced in shallow marine coastal Precambrian successions. Observations made from modern environment as well as Precambrian rock records clearly indicates that the features like petee ridges, sand-cracks, gas domes, multi-directed ripples, reticulate surfaces, sieve-like surfaces and setulf are most likely to form in the shallowest part of the marine basins, in upper intertidal to supratidal conditions while wrinkle structures, roll-up structures and patchy ripples had a broader range of palaeogeographic settings from the supratidal to subtidal conditions. Discoidal microbial colony (DMC) represents a special variety of the mat-layer feature in modern environment that may have diverse internal architecture, sometimes falsely resembles Ediacaran medusoids. The uniqueness in sequence stratigraphic architecture of the microbial mat-covered sediment is reflected by the presence of more amalgamated HSTs compare to that of TSTs. The preservation of forced and normal regressive deposits on low-gradient epeiric shelf under low continental freeboard indicates microbial mat-infested sea-floor impedes erosion and concomitant sediment supply may facilitate formation and preservation of regressive packages.

  13. Fault Zones in the Gulf Coast [gcfltzoneg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — These data represent major fault zones as indicated on Plate 2, Principal structural features, Gulf of Mexico Basin (compiled by T.E. Ewing and R.F. Lopez) in...

  14. Volcanics in the Gulf Coast [volcanicg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The volcanic provinces are modified after Plate 2, Principal structural features, Gulf of Mexico Basin (compiled by T.E. Ewing and R.F. Lopez) in Volume J, The...

  15. Salt Diapirs in the Gulf Coast [gcdiapirg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Locations and shapes of salt diapirs were modified after the New Orleans Geological Society map, Salt tectonism of the U.S. Gulf Coast Basin (compiled by J.A....

  16. José Miguel Jiménez receives Order of Alfonso X the Wise

    CERN Multimedia

    CERN Bulletin

    2016-01-01

    On 12 July 2016, José Miguel Jiménez, Head of CERN Technology Department, has been awarded a spanish civil decoration — an encomienda — of the Order of Alfonso X the Wise (see here), for his outstanding experience in the field of research and scientific management in particle physics.   The ceremony took place at the National Library of Spain, in Madrid, on 12 July. From left: Marcial Marín Hellín, Secretary of State for Education, Professional training and Universities; José María Lassalle Ruiz, Secretary of State for Culture; Íñigo Méndez de Vigo y Montojo, Ministry of Education, Culture and Sport; José Miguel Jiménez, Head of CERN Technology Department; Carmen Vela Olmo, Secretary of State for Investigation, Development and Innovation. (Photo: ©Javier Martínez de la Torre, M...

  17. Adjustment of the basin-scale circulation at 26° N to variations in Gulf Stream, deep western boundary current and Ekman transports as observed by the Rapid array

    Directory of Open Access Journals (Sweden)

    S. A. Cunningham

    2009-10-01

    Full Text Available The Rapid instrument array across the Atlantic Ocean along 26° N provides unprecedented monitoring of the basin-scale circulation. A unique feature of the Rapid array is the combination of full-depth moorings with instruments measuring temperature, salinity, pressure time series at many depths with co-located bottom pressure measurements so that dynamic pressure can be measured from surface to bottom. Bottom pressure measurements show a zonally uniform rise (and fall of bottom pressure of 0.015 dbar on a 5 to 10 day time scale, suggesting that the Atlantic basin is filling and draining on a short time scale. After removing the zonally uniform bottom pressure fluctuations, bottom pressure variations at 4000 m depth against the western boundary compensate instantaneously for baroclinic fluctuations in the strength and structure of the deep western boundary current so there is no basin-scale mass imbalance resulting from variations in the deep western boundary current. After removing the mass compensating bottom pressure, residual bottom pressure fluctuations at the western boundary just east of the Bahamas balance variations in Gulf Stream transport. Again the compensation appears to be especially confined close to the western boundary. Thus, fluctuations in either Gulf Stream or deep western boundary current transports are compensated in a depth independent (barotropic manner very close to the continental slope off the Bahamas. In contrast, compensation for variations in wind-driven surface Ekman transport appears to involve fluctuations in both western basin and eastern basin bottom pressures, though the bottom pressure difference fluctuations appear to be a factor of 3 too large, perhaps due to an inability to resolve small bottom pressure fluctuations after removal of larger zonal average, baroclinic, and Gulf Stream pressure components. For 4 tall moorings where time series dynamic height (geostrophic pressure profiles can be estimated from

  18. Geological Characteristics of Gas Accumulation Combination of Persian Khuff Formation in Gulf Basin%波斯湾盆地Khuff组成藏组合地质特征

    Institute of Scientific and Technical Information of China (English)

    李浩武; 童晓光

    2012-01-01

    The combination of source rock, reservoir and cap rock in the Persian Khuff Formation is the most important gas accumulation combination in the Persian Gulf basin. Both Permian Khuff carbonate and interlayer anhydrite consist in the basic elements of gas accumulation combination of Persian Khuff Formation. The Silurian Qusaiba Formation hot shale is the source rock, with wide distribution, high TOC and moderate thermal maturity at late Craterous. The time of trap formation is earlier than that of hydrocarbon generation window,and many basement faults take vertically a good passageway for hydrocarbon migration from Qusaiba hot shale to Unayzah sandstone and the Unayzah sandstone make a lateral migration passageway. The cyclically deposited anhydrite and carbonates act the good cap rock and high quality reservoir. The Khuff Formation reservoir rocks with good original property are composed of oolite, pellete, hiodetritus packstone and grainstone,with good moldic pore and interparticle pore. The action of leaching and dolomitization greatly improved the reservoir pore at later stage. In most area, the faults do not make the cap rock loss the sealing, so little gas is lost. The potential area of gas exploration is in the overlay area of Qusaiba'Formation mature source rock and interlayer anhydrite, including West Arabian sub-basin, central- east part of Widyan-Mesopotamia sub-basin, northwest of Persian Gulf, and southern area of Ghawar oil field. It is paid more attention in the future to identify the big traps with low closure. Additionally,for the high economy limit of exploration and development in the Middle East, the production for small hydrocar- bon reservoirs need the support of high oil price.%Khuff组成藏组合是波斯湾盆地最重要的天然气成藏组合,二叠系Khuff组储层和层间硬石膏盖层构成了成藏组合的基本要素。下志留统Qusaiba段热页岩是Khuff组成藏组合的烃源岩,其分布广、有机质含量高,在晚

  19. La Segunda Partida de Alfonso X el Sabio y la tradición occidental de los specula principum

    OpenAIRE

    Nanu, Irina

    2013-01-01

    La presente tesis doctoral, titulada La «Segunda Partida» de Alfonso X el Sabio y la tradición occidental de los «specula principum», no es ni pretende ser una monografía tradicional sobre la materia política de la «Segunda Partida»; ni, mucho menos, un repertorio exhaustivo y minucioso de los «specula principum» occidentales, que recogen, en sus enseñanzas, las múltiples inquietudes del pensamiento político medieval, desde el convecionalismo del neoplatonismo agustiniano hasta el naturalism...

  20. El mito de Orestes en Les mouches de Jean-Paul Sartre y El pan de todos de Alfonso Sastre: La necesidad de la acción

    Directory of Open Access Journals (Sweden)

    L. Rovecchio Antón L.

    2012-08-01

    Full Text Available ENIn Les mouches and El pan de todos, Jean-Paul Sartre and Alfonso Sastre speak about the mythological figure of Orestes to reveal the problems of their society. In this article I will focus on the analysis of these two plays and, more specifically, the question of the necessity of the action, which is closely linked with human freedom. A freedom based on choosing a way that leads to direct action or passivity. A choice that, in turn, becomes the essence of human being.Keywords: Jean-Paul Sartre, Alfonso Sastre, Orestes, freedom, action.  ESEn Les mouches y El pan de todos, Jean-Paul Sartre y Alfonso Sastre discurren sobre la figura mitológica de Orestes para revelarnos los problemas de la sociedad que les rodea. En este artículo me centraré en el análisis de estas dos piezas teatrales y, más concretamente, en la cuestión de la necesidad de la acción, que está íntimamente ligada con la libertad del hombre. Una libertad que se basa en la elección de un camino que lleva a la actuación directa o a la pasividad. Una elección que, a su vez, se convierte en la esencia del ser humano.Palabras claves: Jean-Paul Sartre, Alfonso Sastre, Orestes, libertad, acción.

  1. High-resolution seismic stratigraphy of a late Pleistocene submarine fan ponded by salt-withdrawal mini-basins on the Gulf of Mexico continental slope

    Energy Technology Data Exchange (ETDEWEB)

    Winker, C.D.

    1996-12-31

    The late Pleistocene Brazos-Trinity Fan, a structurally ponded fan completely exposed and undisturbed on the seafloor, was mapped with a combination of conventional and high-resolution seismic data. This fan occupies three salt-withdrawal mini-basins (1, 2, 4) and a graben (3), each filled with an onlapping package consisting of alternating bedded and non-bedded units evident on high-resolution data. Basins 1--3 are filled to their topographic spill points; the onlap-fill succession of each is incised by a channel system which bypassed sediment to the next basin(s) downdip. Seismic continuity generally increases distally in the system and within individual basins, believed to reflect the increasing prevalence of turbidity currents over high-density sediment gravity flows.

  2. Simulated Changes in the Ratios of Nutrients Delivered to the Gulf of Mexico in Response to Changes in the Nutrient Sources of Inland Watersheds of the Mississippi River Basin

    Science.gov (United States)

    Alexander, R. B.; Smith, R. A.; Schwarz, G. E.; Boyer, E. W.

    2005-05-01

    Increases in riverine nitrogen loads to the northern Gulf of Mexico have contributed to increased hypoxia in the coastal waters of the Louisiana shelf during the past several decades. Nitrogen is the most limiting nutrient for algal production in these waters, however, Mississippi River nutrient loads entering the Gulf are closely balanced with seasonally shifting Redfield ratios. Moreover, state concerns over phosphorus, which is generally more limiting to primary production in inland waters, may contribute to an increased emphasis on future phosphorus reductions to meet designated use requirements in state waters. Currently, knowledge is lacking about how nutrient ratios in Mississippi River loads are likely to respond to future changes in nutrient sources in inland watersheds. An improved understanding is initially needed of the major sources and processes in the Mississippi River Basin (MRB) that control both phosphorus and nitrogen delivery to the Gulf. Earlier modeling studies of nutrients in the MRB have focused primarily on nitrogen with little attention to phosphorus. Here, we develop a Spatially Referenced Regression on Watershed Attributes (SPARROW) model of mean-annual total phosphorus (TP) loads for streams in the MRB. The SPARROW model links measurements of TP loads in streams with geographic data on phosphorus sources (e.g., fertilizer, livestock wastes, urban sources) and properties of the landscape that influence transport (e.g., climate, topography, vegetation, soils, water routing). The model employs mechanistic components and mass balance constraints within a formal parameter-estimation structure to empirically quantify the sources, attenuation rates, and transport of phosphorus in the terrestrial and aquatic ecosystems of the MRB. The model was used to quantify the interior watersheds and nutrient sources that contribute to phosphorus delivery to the Gulf. Using a previously estimated SPARROW nitrogen model for the MRB, we computed Redfield

  3. Deglacial nitrogen isotope changes in the Gulf of Mexico: Evidence from bulk sedimentary and foraminifera-bound nitrogen in Orca Basin sediments

    OpenAIRE

    A. N. Meckler; Ren, H.; Sigman, D. M.; Gruber, N.; Birgit Plessen; Schubert, C. J.; Haug, G.H.

    2011-01-01

    Constraining variations in marine N(2)-fixation over glacial-interglacial timescales is crucial for determining the role of the marine nitrogen cycle in modifying ocean productivity and climate, yet paleo-records from N2-fixation regions are sparse. Here we present new nitrogen isotope (delta(15)N) records of bulk sediment and foraminifera test-bound (FB) nitrogen extending back to the last ice age from the oligotrophic Gulf of Mexico (GOM). Previous studies indicate a substantial terrestrial...

  4. Alfonso VI en la Estoria de Espanna: Retrato ejemplar y narración histórica

    Directory of Open Access Journals (Sweden)

    Aníbal A. Biglieri

    2001-11-01

    Full Text Available Alfonso VI's figure is presented in the Estoria de Espanna through two different types of discourse: the initial portrait, where he is described as an exemplary king (chapter 846, according to the image of the ideal statesman given on the second Partida, and his reign's account, which reveals a far more complex and contradictory personality. The opposition between non-temporality = individuality raises, among many others, two main problems to the understanding of the alphonsine historian workshop: the conception of human personality, within the framework of the "discovery of the individual" process -studied by Morris (1987-, and the comprehension of unique and unrepeatable historical facts, enlightened by principles and general categories.

  5. Cultura e política: José Vasconcelos e Alfonso Reyes no Brasil (1922-1938

    Directory of Open Access Journals (Sweden)

    Regina Aída Crespo

    2003-07-01

    Full Text Available De 1922 a 1938, as relações culturais entre o México e o Brasil conheceram um momento particularmente fecundo, devido em grande parte à atuação de dois intelectuais mexicanos: José Vasconcelos e Alfonso Reyes. A ausência de uma tradição de intercâmbio cultural entre o México e o Brasil fez do âmbito diplomático um espaço fundamental para a aproximação entre os dois países. Como representantes do governo mexicano - e transitando entre as fronteiras muitas vezes difusas da cultura e da política -, Vasconcelos, em 1922, e Reyes, de 1930 a 1938, estabeleceram uma ampla rede de contatos com intelectuais brasileiros e conseguiram fazer do México uma referência cultural e política importante no Brasil, durante o período.From 1922 to 1938, cultural relations between Mexico and Brazil had a particularly rich moment basically due to two Mexican intellectuals: José Vasconcelos and Alfonso Reyes. There was no tradition of cultural interchange between Mexico and Brazil; so the diplomatic sphere was transformed into a fundamental space for the approximation between these two countries. As representatives of the Mexican government - traveling between the frequently diffuse boundaries of culture and politics - Vasconcelos, in 1922, and Reyes, from 1930 to 1938, established a wide network of contacts with Brazilian intellectuals and managed to make Mexico an important cultural reference in Brazil, during that period.

  6. RRS "Charles Darwin" Cruise CD166, 29 Oct - 22 Nov 2004. Sedimentary processes and deposits in the Agadir Basin and Gulf of Cadiz

    OpenAIRE

    Wynn, R.B.; Cronin, B.T.

    2005-01-01

    The primary aim of CD166 was to undertake intensive coring in the Agadir Basin on the Northwest African margin, with the intention of characterising deep-water gravity flow processes and deposits at a basin-wide scale. In addition, it was hoped that sampling of volcaniclastic turbidites derived from Canary Islands landslides would provide insights into landslide processes and aid assessment of potential tsunami hazards. In addition, the first two days of the cruise were assigned to piston cor...

  7. Limit of Salt in the Gulf Coast [saltlimitg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The data provides the approximate limit of Middle Jurassic salt from Plate 2, Principal structural features, Gulf of Mexico Basin (compiled by T.E. Ewing and R.F....

  8. Preliminary Basin Analysis of Latest Miocene Conglomerate Near Bahía Kino, Coastal Sonora: A New Record of Crustal Deformation During Initial Opening of the Northern Gulf of California

    Science.gov (United States)

    Dorsey, R. J.; Peryam, T. C.; Bennett, S.; Oskin, M. E.; Iriondo, A.

    2008-12-01

    In coastal Sonora northwest of Bahía Kino, we have initiated a basin-analysis study of nonmarine conglomerate (Tcg) that overlies and is locally interbedded with the 6.4-Ma Tuff of Mesa Cuadrada (Tmc). Tcg conglomerate is deeply eroded and cut by a complex set of syn- to post-basinal, N- to NNE-striking normal faults and NW-striking dextral strike-slip faults. We carried out detailed mapping and field descriptions, measured stratigraphic sections, and collected paleocurrent and clast-count data in Tcg. Zircons from the newly discovered Seri tuff near the base of the section, 160 m below Tmc, were dated using U-Pb SHRIMP geochronology at Stanford University. We obtained a 206Pb/238U weighted mean age of 6.53+/-0.18 Ma (n=14; MSWD=1.3), which yields a sediment-accumulation rate of 0.8+/-0.2 mm/yr for lower Tcg. Tcg is dominated by debris-flow facies consisting of massive, poorly sorted, weakly bedded, matrix-rich, pebble, cobble, to small-boulder conglomerate. A subsidiary sheet-flood facies is somewhat better sorted, generally lacks boulders, and contains weak but pervasive horizontal stratification. Both facies of Tcg record deposition in an alluvial fan environment. Well sorted and stratified stream deposits are conspicuously lacking. Preserved sections of Tcg range up to 170 to 240 meters thick in the southern part of the study area, and increase to at least 470 meters in the north where the Punta Chueca fault, a large NW-directed low-angle normal fault, apparently produced more extension and subsidence than smaller faults in the south. Clasts in Tcg are dominated by middle Miocene andesite, the 12.6-Ma Tuff of San Felipe, minor amounts of Tmc, and variable amounts of older basement rocks including tonalite, granodiorite, quartzite, metavolcanic rock, and a megacrystic K-spar-bearing granite that we have not seen in the local bedrock. After correcting for bedding dips and vertical-axis clockwise rotations determined from paleomagnetic analysis, restored

  9. Un paso de América: Alfonso Reyes, Victoria Ocampo y el cosmopolitismo en la década de 1930 / Un paso de América: Alfonso Reyes, Victoria Ocampo and the Cosmopolitanism in the 1930’s

    Directory of Open Access Journals (Sweden)

    Gorica Majstorovic

    2014-12-01

    Full Text Available El artículo trata de las construcciones americanistas del cosmopolitismo (entendido en relación a la geopolítica imperial en los textos de Victoria Ocampo y Alfonso Reyes de los años treinta. Al analizar su relación con los movimientos de inmigración y la subsiguiente revalorización de la nación, el artículo postula que en Alfonso Reyes la mediación cosmopolita es «des-jerarquizada», ubicada casi siempre en una «periferia», a diferencia de Victoria Ocampo cuyas visiones cosmopolitas son mediadas desde un «centro» —ya sea París o Buenos Aires— y relacionadas con una jerarquía de valores estéticos y políticos.The article deals with Americanist constructions of cosmopolitanism (understood in relation to the imperial geopolitics in the texts of Victoria Ocampo and Alfonso Reyes in the 1930’s. Upon analyzing its relationship with immigration movements and the subsequent revaluation of the nation, the article suggests that in Alfonso Reyes cosmopolitan mediation is «dis-hierarchized», almost always located in a periphery, unlike Victoria Ocampo whose cosmopolitan visions are mediated from a «center» —either Paris or Buenos Aires— and related to a hierarchy of aesthetic and political values.

  10. Martinez Arranz, Alfonso / Doyle, Natalie J. / Winand, Pascaline (eds.), New Europe, New World? The European Union, Europe and the Challenges of the 21 st Century,

    OpenAIRE

    Adrian IVAN

    2010-01-01

    New Europe, New World? The European Union, Europe, and the Challenges of the 21 st Century is a collective work that emerged from such an academic engagement generated by the Monash European and EU Center (at Monash University, Australia) in collaboration with the Austral-Asian Center for Italian Studies. The editors, Alfonso Martinez Arranz, Natalie J. Doyle and Pascaline Winand, succeeded in turning the conference debates into a coherent volume that will certainly contribute to the academic...

  11. Faults in the Gulf Coast [gcfaultsg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — These mapped faults are modified from Plate 2, Principal structural features, Gulf of Mexico Basin (compiled by T.E. Ewing and R.F. Lopez) in Volume J, The Geology...

  12. Alfonso Reyes en dos tiempos. Entre el arielismo y la doble experiencia literaria: "La venganza creadora" y "La cena"

    Directory of Open Access Journals (Sweden)

    Pablo Aparicio Durán

    2013-06-01

    Full Text Available Es sabido que Alfonso Reyes dejó una enorme impronta intelectual y literaria no sólo en la literatura de su país, Méjico, sino en toda la literatura hispanoamericana. Pero, aparte de las dimensiones de la huella dejada por el autor, lo realmente interesante es el terreno que pisa, y ese, para nosotros, es el terreno ideológico. Así, en el presente artículo ofrecemos una panorámica general sobre la significación cultural del autor mejicano, precisamente para tratar de delimitar que una cosa son las ideologías culturales explícitas y otra cosa es el inconsciente ideológico/literario implícito. En este sentido, se ha efectuado el análisis de dos cuentos del prolífico escritor de Monterrey (La venganza creadora y La cena en relación con otros dos de Edgar Allan Poe y Ernest Hemingway (Allá en Michigan y La casa Usher, respectivamente.

  13. Alfonso IX de León y el iter de su corte (1188-1230

    Directory of Open Access Journals (Sweden)

    Gregoria CAVERO DOMÍNGUEZ

    2009-12-01

    Full Text Available Alfonso IX de León, a lo largo de su dilatado reinado, desarrolló la mayor parte de las actividades de la corte de forma itinerante, es decir en medio de sus largos y continuados desplazamientos, tal como reflejan las datas de los documentos de su cancillería. La ciudad de León, sede regia, no fue el epicentro de su corte, aunque en ella se desarrollaran las primeras cortes.La majeure partie des activités du roi de León Alphonse IX se déroulèrent, au cours de son long règne, de façon itinérante, c’est-à-dire au cours de ses longs déplacements, comme le réflètent les données documentaires de sa chancellerie. La ville de León, siège royal, ne fut pas l’épicentre de sa cour, mais accueillit pourtant les premières cortes.

  14. Gulf War

    DEFF Research Database (Denmark)

    Dalgaard-Nielsen, Anja

    2003-01-01

    As it became a non‐permanent member of the UN Security Council in January 2003, Germany stepped up its opposition to war with Iraq. The stage was set for a repeat of Germany's uncomfortable position during the 1991 Gulf War. At that time, as most of Germany's allies rallied behind Washington......, Germany made only financial contributions, and hundreds of thousands of Germans took to the streets to protest against the war. Yet, since 1991, Germany had come a long way in its attitudes towards military force. From a policy of complete abstention from military deployments beyond NATO's area (so...

  15. Coastal fisheries in the Eastern Baltic Sea (Gulf of Finland and its basin from the 15 to the Early 20th centuries.

    Directory of Open Access Journals (Sweden)

    Julia Lajus

    Full Text Available The paper describes and analyzes original data, extracted from historical documents and scientific surveys, related to Russian fisheries in the southeastern part of the Gulf of Finland and its inflowing rivers during the 15- early 20(th centuries. The data allow tracing key trends in fisheries development and in the abundance of major commercial species. In particular, results showed that, over time, the main fishing areas moved from the middle part of rivers downstream towards and onto the coastal sea. Changes in fishing patterns were closely interrelated with changes in the abundance of exploited fish. Anadromous species, such as Atlantic sturgeon, Atlantic salmon, brown trout, whitefish, vimba bream, smelt, lamprey, and catadromous eel were the most important commercial fish in the area because they were abundant, had high commercial value and were easily available for fishing in rivers. Due to intensive exploitation and other human-induced factors, populations of most of these species had declined notably by the early 20(th century and have now lost commercial significance. The last sturgeon was caught in 1996, and today only smelt and lamprey support small commercial fisheries. According to historical sources, catches of freshwater species such as roach, ide, pike, perch, ruffe and burbot regularly occurred, in some areas exceeding half of the total catch, but they were not as important as migrating fish and no clear trends in abundance are apparent. Of documented marine catch, Baltic herring appeared in the 16(th century, but did not become commercially significant until the 19(th century. From then until now herring have been the dominant catch.

  16. Basin Analysis of the Mississippi Interior Salt Basin and Petroleum System Modeling of the Jurassic Smackover Formation, Eastern Gulf Coastal Plain, Final Report and Topical Reports 5-8 on Smackover Petroleum system and Underdevelopment Reservoirs

    Energy Technology Data Exchange (ETDEWEB)

    Mancini, Ernest A.; Puckett, T. Markham; Parcell, William C.; Llinas, Juan Carlos; Kopaska-Merkel, David C.; Townsend, Roger N.

    2002-03-05

    The Smackover Formation, a major hydrocarbon-producing horizon in the Mississippi Interior Salt Basin (MISB), conformably overlies the Norphlet Formation and is conformably overlain by the Buckner Anhydrite Member of the Haynesville Formation. The Norphlet-Smackover contact can be either gradational or abrupt. The thickness and lithofacies distribution of the Smackover Formation were controlled by the configuration of incipient paleotopography. The Smackover Formation has been subdivided into three informal members, referred to as the lower, middle and upper members.

  17. Seimic Images and Wide-angle Velocity constrains of the structure and geodynamic origin of the Gibraltar Arc system: A geological interpretation of the Gulf of Cadiz imbricated wedge, the western and eastern Alboran basins, and the South-Balearic basin.

    Science.gov (United States)

    Gracia, E.; Ranero, C. R.; Grevemeryer, I.; WestMed, TopoMed, , T. h. e.; cruise parties, Geomargen-1

    2012-04-01

    The current geodynamics of the region between north Africa and the Iberian Peninsula are dominated by the collision between the Eurasian and African plates. The ongoing deformation is mainly driven by the NW-SE, slow 4-5 mm/yr convergence that is partitioned across numerous faults and diffused through a broad region with no clear plate boundary defined. However, this region is characterized by the a series of geological structures that appear unrelated to the current dominant plate kinematics. The region is formed by the Gibraltar Arc system, an arcuate structure that is fronted by a large imbricated wedge of tectonically piled sediment slices in the Gulf of Cadiz, and a series of basins in the Mediterranean part of the region. The western, little deformed Alboran basin is located on the rear of the Gibraltar stacked units. The eastern Alboran basin is characterized by numerous volcanic ridges and is transitional to the South Balearic - North Algerian basin that displays a generally lower topography. The different tectonic elements are floored by a poorly known crystalline basement and their age, evolution and geodynamic origin is still strongly debated. Part of the uncertainty arises from the lack of deep penetrating modern geophysical data in much of the region. In the last 5 years, 3 successive cruise in the region have produced an extensive coverage of the different tectonic elements collection a series of wide angle seismic profiles in 2006 during the WestMed cruise with German R/V Meteor and two multichannel seismic reflection cruises with the R/V Sarmiento de Gamboa from mid September to late October (TopoMed-Gassis cruise) and late October to late November (Geomargen-1 cruise) 2011. In this contribution we present the new images of the tectonic structures and sedimentary basin and the wide-angle seismic velocity models across key regions of the system. We also present an interpretation of the entire system in the context of a geodynamic model of eastward

  18. La empresa informativa y el poder de informar, según la perspectiva de tres autores contemporáneos: Alfonso Nieto, Niklas Luhmann y Roberto Marafioti

    OpenAIRE

    Rodríguez Rowe, Verónica

    2015-01-01

    El origen de la tesis es el estudio de la visión de autores contemporáneos, de distinta nacionalidad y profesión, respecto a un tema siempre contingente: la empresa informativa y el poder de informar. Se exploraron las aportaciones del español Alfonso Nieto, el alemán Niklas Luhmann y el argentino Roberto Marafioti. Se evidenciaron distintas posiciones respecto al rol de los mass media. Así Luhmann1 precisa que constituyen una forma de comunicación que se emplaza en el mismo nivel de operaci...

  19. Antecedentes y creación del Instituto de Sueroterapia, Vacunación y Barteriología de Alfonso XIII

    OpenAIRE

    Porras Gallo, María Isabel

    1998-01-01

    En el presente trabajo, utilizando como fuente primordial una selección de la prensa general y de la científico-profesional médica y farmacéutica, se estudia el proceso de constitución del Instituto de Sueroterapia, Vacunación y Bacteriología de Alfonso XIII en 1899. Mediante el análisis de los antecedentes y orígenes de la citada institución se intenta poner de relieve los principales factores que influyeron en su gestación y desarrollo posterior, y se muestra en qué circunstancias se produj...

  20. Alfonso de Palencia. Ad Alfonsum de Velasco in funebrem Abulensis praesulis fabulosa narratio (ca. 1455: edición crítica del MS UCM BH 133

    Directory of Open Access Journals (Sweden)

    Durán Barceló, Javier

    2012-01-01

    Full Text Available Aunque ya estaba catalogado desde 1745 y de nuevo en 1800, los modernos estudiosos no tuvieron noticia de la existencia de este manuscrito del siglo XV de Alfonso de Palencia hasta que Bartolomé José Gallardo lo describió. Gallardo describe el manuscrito Ad Alfonsum de Velasco in funebrem Abulensis praesulis cuando éste se encontraba a modo de préstamo en la Real Academia de la Historia, en Madrid, a mediados del siglo XIX. En aquella época la RAH procuraba la publicación de las obras de Alfonso de Palencia y seguramente a aquellos esfuerzos se debe que se conserve actualmente en la RAH una copia moderna de este manuscrito medieval, el cual fue devuelto a su propietaria. La primera edición del texto la hicieron en 1982 Brian Tate y Rafael Alemany Ferrer basándose para ello en la copia decimonónica. Pues, dado que Gallardo había dado una información confusa acerca de la localización del manuscrito medieval, los modernos editores no pudieron localizarlo. Este trabajo resuelve finalmente el problema de la localización del manuscrito original, conservado en la Universidad Complutense de Madrid. Gracias a este hallazgo mi edición del texto se basa directamente en el original medieval sobre el que intento dilucidar algunas lecturas difícilesAlthough it had been catalogued in 1745 and again in 1800, it was not until Bartolomé José Gallardo reported the existence of this 15th century manuscript of Alfonso de Palencia when scholars became aware of its existence. Gallardo described the manuscript Ad Alfonsum de Velasco in funebrem Abulensis praesulis when it was borrowed by the Royal Academy of History, in Madrid, in mid 19th century. At that time the Academy was involved in the edition of the works of Alfonso de Palencia and for this reason a hand written copy of the medieval manuscript remained in the Academy, while the original was returned to its owner. Based on this 19th century copy, Brian Tate and Rafael Alemany Ferrer published

  1. Comunicar para el cambio social: una comunicación ética y política. Entrevista con Alfonso Gumucio Dagron

    OpenAIRE

    Gabriel Jaime Pérez S.J.; Mónica Marion Cataño; Fanny Patricia Franco

    2009-01-01

    En este artículo, a partir de sus experiencias académicas y laborales, Alfonso Gumucio Dagron define el concepto comunicación para el cambio social como el planteamiento más reciente de las teorías de la dependencia y de los enfoques de la comunicación. Él sostiene que se centra en la sistematización de experiencias, porque facilita recuperar el conocimiento producido en el diálogo social, a partir de lecciones narradas y aprendidas por las comunidades. Así mismo, sostiene que la metodología ...

  2. El redescubrimiento de la otredad: nuevas perspectivas sobre el descubrimiento de la conquista en Caminarás con el sol de Alfonso Mateo Sagasta

    Directory of Open Access Journals (Sweden)

    Francesca Crippa

    2013-07-01

    Full Text Available RESUMEN: Alfonso Mateo-Sagasta es uno de los autores más representativos del panorama literario español actual. Su última novela, Caminarás con el sol, aborda uno de los episodios más controvertidos de la historia española e hispanoamericana a través del punto de vista de un hombre, Gonzalo Guerrero, que decidió abandonar sus tradiciones para convertirse en guerrero maya. La finalidad de este trabajo es analizar los principales recursos temáticos y estilísticos de la obra de Mateo-Sagasta en relación con la específica época histórica de ambientación de la novela. ABSTRACT: Alfonso Mateo-Sagasta is one of the most popular authors of the present Spanish literary panorama. His last novel, Caminarás con el sol, approaches one of the most debated episodes of the Spanish and Latin American history by adopting the point of view of a man, Gonzalo Guerrero, who decided to renounce to his own culture in order to become a Mayan warrior. The aim of this article is to analyze the main thematic and stylistic features of Mateo-Sagasta’s novel and its approach to the specific historical period.

  3. Vejamen de Alfonso de Batres para la Academia de 1638 (Manuscrito inédito. Estudio y edición crítica

    Directory of Open Access Journals (Sweden)

    Julio, Teresa

    2013-06-01

    Full Text Available During February 1638 the Fiestas de Carnestolendas were celebrated at the Buen Retiro Palace, Madrid. Among the programmed activities, a literary gathering was held, open to numerous poets and courtiers. From this gathering three vejamenes have been preserved: those of Alfonso de Batres, Antonio Coello and Francisco de Rojas Zorrilla. In this paper we analyze and annotate the vejamen that Batres read before His Majesties in the Royal Salon of the Retiro Palace on February 11, 1638.Durante el mes de febrero de 1638 se celebraron en el palacio del Buen Retiro las fiestas de Carnestolendas. Entre las actividades programadas, se realizó una academia literaria en la que participaron poetas y cortesanos. De ella se conservan tres vejámenes: el de Alfonso de Batres, el de Antonio Coello y el de Francisco de Rojas Zorrilla. En el presente artículo se analiza y edita críticamente el vejamen que Batres defendió ante sus majestades en el Salón Real del Retiro el 11 de febrero de 1638.

  4. Last millennium sedimentation in the Gulf of Cariaco (NE Venezuela): Evidence for morphological changes of gulf entrance and possible relations with large earthquakes

    Science.gov (United States)

    Aguilar, Iliana; Beck, Christian; Audemard, Franck; Develle, Anne-Lise; Boussafir, Mohammed; Campos, Corina; Crouzet, Christian

    2016-01-01

    The Cariaco Basin and the Gulf of Cariaco in Venezuela are two major basins along the seismogenic El Pilar right lateral fault, among which the Cariaco Basin is a pull-apart. Both basins are sites of anoxia and organic-rich deposits. To examine whether the sediments in the Gulf of Cariaco have recorded traces of historical or prehistorical earthquakes, we extracted and analyzed twelve 1 m-long gravity cores, sampling the last millennium sedimentation. We focused on analyzing the sediment sources with different techniques (particle size analysis, XRF, loss on ignition tests, magnetic properties, Rock-Eval pyrolysis, 14C dating). The results confirm that major upwelling occurs at the western gulf entrance and makes deep water flowing from the Cariaco Basin into the Gulf of Cariaco. These flows carry an organic-rich suspended load. Furthermore, we found evidence of a particular, widespread fine-grained siliciclastic deposit (named SiCL3) within the gulf, whose age suggests that it likely formed during the large 1853 AD earthquake that stroke the Cumaná city. We suggest that the earthquake-induced large submarine landslides that modified the topography of the gulf's entrance, which in turn promoted upwelling and open marine water flows from the Cariaco Basin. The layer SiCL3 would be the sediment load remobilized during this chain of events.

  5. Prólogo arameo y anotaciones hebreas de Alfonso de Zamora para una copia manuscrita del Targum a los Profetas encargada por la Universidad de Salamanca

    Directory of Open Access Journals (Sweden)

    Fontela, Carlos Alonso

    2009-12-01

    Full Text Available University Library Ms. Or. 645, f. 110r (ol. Warner 65 F contains, besides a draft for an Aramaic prologue to the work on Targum written by Alonso de Zamora ca. 1532, additional notes written by himself dealing with the comission he received to copying Targumic texts. The present article improves the edition of the Aramaic prologue, previously published by Neubauer (1895, offering a Spanish translation and the edition of the marginal notes, that contain a draft of the prayers (תפלותופיהספדים for the partial colophons of the books of Ezekiel, Hosea and Joel’s Targums. These pa - tial colophons in the Leiden Ms. coincide with the clean drafts by Zamora preserved in an autograph manuscript, Salamanca University Library Ms. M-3 (Est.-1, Cajón I-Núm. 2. An explanation concerning additional annotations (the incipit of Isaiah 57, that spoiled the folio, and led it to its being re-used by Alonso de Zamora as a draft.

    El ms. Or. 645, f.º 110r (ol. Warner 65 F de la Leiden University Library, además del borrador de un prólogo arameo a la obra de Targum escrito por Alfonso de Zamora hacia el año 1532 por encargo de la Universidad de Salamanca, contiene otras anotaciones del mismo autor que aquí se publican por primera vez y que también formaban parte del mismo encargo de copia de textos targúmicos. En el presente artículo, además de mejorar el texto arameo del prólogo ya publicado por Neubauer en 1895, se ofrece su traducción española por primera vez. Asimismo, se publica y traduce una anotación marginal que consiste en un borrador de las jaculatorias o doxologías (תפלותופיהספדים para los colofones parciales de los libros del Targum de Ezequiel, Oseas y Joel. Estos colofones parciales del ms. de Leiden coinciden con los pasados a limpio que se conservan en el manuscrito autógrafo de Alfonso de Zamora ms. M-3 (Est.-1, Cajón I-Núm. 2 de la Biblioteca Universitaria de Salamanca. Se

  6. Gulf Canada's Russian joint venture

    International Nuclear Information System (INIS)

    After three years of evaluating prospects and negotiating with government and industry representatives, Gulf Canada established its first joint venture in the Russian Federation with Komineft, a production association from the Komi autonomous republic. Komineft has a 50% share of the venture, and the rest is shared equally between Gulf and British Gas. The operating area is at the Vozey and Upper Vozey fields in the Timan-Pechora Basin, some 1,500 km northeast of Moscow just inside the Arctic Circle. An attractive feature of the Upper Vozey project is low development costs of ca $2/bbl. In the Vozey field, the venture will set up an enhanced oil recovery demonstration project to test techniques perfected in Alberta. About 60 Canadians are involved on the project, and headquarters are in Usinsk, ca 100 km south of the oil fields. In the first half of 1992, oil production in the first phase of the venture averaged around 10,000 bbl/d and continues to increase

  7. Beyond the Gulf Metropolises

    DEFF Research Database (Denmark)

    Wippel, Steffen

    2013-01-01

    The extended studies on urbanisation in the Gulf region that came up in the early 2000s concentrated on the main centres with their worldwide-admired mega-projects and branding strategies. Only rather recently did a more general interest arise in the second-tier range of Gulf cities, which also s...

  8. AEROBIC DENITRIFICATION: IMPLICATIONS FOR THE MOM RIVER BASIN

    Science.gov (United States)

    Each year about 1.6 million metric tons of nitrogen, mostly from agriculture, is discharged from the lower Mississippi/Atchafalaya River Basin into the Gulf of Mexico, and each spring this excess nitrogen fuels the formation of a huge hypoxic zone in the Gulf. In the Mississippi...

  9. Rings dominate western Gulf

    Science.gov (United States)

    Vidal L., Francisco V.; Vidal L., Victor M. V.; Molero, José María Pérez

    Surface and deep circulation of the central and western Gulf of Mexico is controlled by interactions of rings of water pinched from the gulf's Loop Current. The discovery was made by Mexican oceanographers who are preparing a full-color, 8-volume oceanographic atlas of the gulf.Anticyclonic warm-core rings pinch off the Loop Current at a rate of about one to two per year, the scientists of the Grupo de Estudios Oceanográficos of the Instituto de Investigaciones Eléctricas (GEO-IIE) found. The rings migrate west until they collide with the continental shelf break of the western gulf, almost always between 22° and 23°N latitude. On their westward travel they transfer angular momentum and vorticity to the surrounding water, generating cyclonic circulations and vortex pairs that completely dominate the entire surface and deep circulation of the central and western gulf.

  10. Vides de Simón de Rojas Clemente (1777-1827 en el herbario del Real Colegio Alfonso XII de San Lorenzo de El Escorial (Madrid, España

    Directory of Open Access Journals (Sweden)

    Perea, Domingo

    1997-12-01

    Full Text Available In the present paper, the discovery of grape-vine mounted sheets from the Simón de Rojas Clemente herbarium, which were found in the Herbarium of the Real Colegio Alfonso XH in San Lorenzo de El Escorial, is reported. This material completes the collection of Clemente's vines which makes up one of the historical collections deposited in the MA herbarium.Damos a conocer unos pliegos de vides procedentes del herbario de Simón de Rojas Clemente que han aparecido en el Gabinete de Ciencias Naturales del Real Colegio Alfonso XII de San Lorenzo de El Escorial. Estos materiales completan la colección de vides de Clemente que constituye uno de los herbarios históricos depositados en MA.

  11. Evaluation of the economic costs and benefits of methods for reducing nutrient loads to the Gulf of Mexico: Topic 6 Report for the Integrated Assessment on Hypoxia in the Gulf of Mexico.

    OpenAIRE

    Doering, Otto C., III; Diaz-Hermelo, Francisco; Howard, Crystal; Heimlich, Ralph; Hitzhusen, Fred; Kazmierczak, Richard; Lee, John; Libby, Larry; Milon, Walter; Prato, Tony; Ribaudo, Marc

    1999-01-01

    In this report we analyze the Topic 5 report’s recommendations for reducing nitrogen losses to the Gulf of Mexico (Mitsch et al. 1999). We indicate the relative costs and cost-effectiveness of different control measures, and potential benefits within the Mississippi River Basin. For major nonpoint sources, such as agriculture, we examine both national and basin costs and benefits. Based on the Topic 2 economic analysis (Diaz and Solow 1999), the direct measurable dollar benefits to Gulf...

  12. Gulf Shrimp System

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Gulf of Mexico Shrimp Landings - This data set contains catch (landed catch) and effort for fishing trips made by the larger vessels that fish near and offshore for...

  13. Gulf operations still recovering

    International Nuclear Information System (INIS)

    This paper reports that reports of damage caused by Hurricane Andrew were leveling off last week at the U.S. Minerals Management Service as Gulf of Mexico operators pressed ahead with repairs. The hurricane struck South Florida Aug. 4, churned west into the gulf, then swung north and hit the South Louisiana coast Aug. 5. By the close of business Sept. 8 MMS had received damage reports covering 83 pipeline segments and 193 platforms and satellite installations. MMS last week estimated about 500 MMcfd of gas production had been restored in the gulf and 100,000-150,000 b/d of oil. Production still lost as a result of Andrew was estimated at 2-2.5 bcfd of gas and 90,000-120 b/d of oil. MMS estimates Gulf of Mexico wells before the storm were producing about 12.5-13 bcfd of gas and 750,000 b/d of oil

  14. Gulf of Alaska, Alaska

    Science.gov (United States)

    2002-01-01

    This MODIS true-color image shows the Gulf of Alaska and Kodiak Island, the partially snow-covered island in roughly the center of the image. Credit: Jacques Descloitres, MODIS Land Rapid Response Team

  15. 2014 Gulf of Mexico Hypoxia Forecast

    Science.gov (United States)

    Scavia, Donald; Evans, Mary Anne; Obenour, Dan

    2014-01-01

    The Gulf of Mexico annual summer hypoxia forecasts are based on average May total nitrogen loads from the Mississippi River basin for that year. The load estimate, recently released by USGS, is 4,761 metric tons per day. Based on that estimate, we predict the area of this summer’s hypoxic zone to be 14,000 square kilometers (95% credible interval, 8,000 to 20,000) – an “average year”. Our forecast hypoxic volume is 50 km3 (95% credible interval, 20 to 77).

  16. 2013 Gulf of Mexico Hypoxia Forecast

    Science.gov (United States)

    Scavia, Donald; Evans, Mary Anne; Obenour, Dan

    2013-01-01

    The Gulf of Mexico annual summer hypoxia forecasts are based on average May total nitrogen loads from the Mississippi River basin for that year. The load estimate, recently released by USGS, is 7,316 metric tons per day. Based on that estimate, we predict the area of this summer’s hypoxic zone to be 18,900 square kilometers (95% credible interval, 13,400 to 24,200), the 7th largest reported and about the size of New Jersey. Our forecast hypoxic volume is 74.5 km3 (95% credible interval, 51.5 to 97.0), also the 7th largest on record.

  17. Comunicar para el cambio social: una comunicación ética y política. Entrevista con Alfonso Gumucio Dagron

    Directory of Open Access Journals (Sweden)

    Gabriel Jaime Pérez S.J.

    2009-01-01

    Full Text Available En este artículo, a partir de sus experiencias académicas y laborales, Alfonso Gumucio Dagron define el concepto comunicación para el cambio social como el planteamiento más reciente de las teorías de la dependencia y de los enfoques de la comunicación. Él sostiene que se centra en la sistematización de experiencias, porque facilita recuperar el conocimiento producido en el diálogo social, a partir de lecciones narradas y aprendidas por las comunidades. Así mismo, sostiene que la metodología más adecuada para dinamizar experiencias de comunicación para el cambio social es la investigación acción-participativa (iap, porque permite investigar y acompañar procesos desde el conocimiento académico y profesional en dinámicas de participación, diálogo y construcción colectiva.

  18. Gulf Island National Wildlife Refuges

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This document provides a brief history and describes physical features of the Gulf Island National Wildlife Refuges. The Gulf Island National Wildlife Refuges...

  19. Geologic evolution of the continental margin of the Gulf of Tehuantepec in Southwestern Mexico

    Science.gov (United States)

    Sanchez-Barreda, L. A.

    Through the use of surface geology, paleomagnetic data, gravity surveys, and continuous seismic reflection profiles, the evolution of the Gulf of Tehuantepec is detailed as a progression from an open ocean basin to a more restricted basinal setting. Paleomagnetic data from the Mexican states of Chiapas and Oaxaca suggest an equatorial location for the Yucatan block during the Permian. The Gulf of Tehuantepec and its associated coastal plain is divided into three regions based on the character and distribution of the gravity anomalies. The differences in these regions suggest a northerly increase in tectonic activity in the basin and the coastal plain. A possible extension of the Polochic fault into the Gulf of Tehuantepec is indicated by coincidence of a linear trend of gravity anomalies in the southern coastal plain with the westernmost end of the fault.

  20. Alfonso López Pumarejo y la última Corte Suprema de Justicia de la hegemonía conservadora, 1934-1935

    Directory of Open Access Journals (Sweden)

    Mario Alberto Cajas Sarria

    2013-01-01

    Full Text Available Este artículo analiza las relaciones entre el Ejecutivo y la Corte Suprema de Justicia de Colombia durante el primer año de gobierno del presidente liberal Alfonso López Pumarejo, entre 1934 y 1935, cuando este lidió con un tribunal integrado por una mayoría de magistrados pertenecientes al Partido Conservador, que era percibido como el último bastión de la hegemonía conservadora. Este trabajo pone en evidencia el comportamiento estratégico de una Corte Suprema dominada por magistrados de origen conservador, que parecía intentar una relación institucional de colaboración con el nuevo gobierno hacia el año 1934. Reconstruye el juicio de constitucionalidad a la reforma tributaria impuesta por decreto de estado de sitio del Ejecutivo liberal que la Corte declaró inexequible en 1935, cuya decisión generó que la corporación fuera percibida como un órgano que actuaba movido por intereses partidistas. Por último, ofrece un análisis en conjunto sobre el rol político del tribunal en esta coyuntura del régimen político colombiano. Este análisis busca contribuir a una mejor comprensión del control constitucional colombiano y del rol que jugó la Corte Suprema de Justicia como juez constitucional –y por tanto, actor del régimen político–, en una perspectiva histórica, en este caso en el contexto de la transición de la hegemonía conservadora a la Segunda República Liberal que se consolidó con el gobierno de la Revolución en Marcha.

  1. The lower atmosphere over the Gulf of California

    Science.gov (United States)

    Badan-Dangon, Antoine; Dorman, Clive E.; Merrifield, Mark A.; Winant, Clinton D.

    1991-09-01

    Automated meteorological observations at coastal and island stations, instrumented aircraft flights, and coastal soundings were made between July 1983 and June 1985 to define the variations of the lower atmosphere over the northern half of the Gulf of California during the two important climatic seasons, the mid-latitude winter and the subtropical summer. A marine layer is well defined over water during both seasons but dissipates within a few kilometers inland. The winter large-scale pressure field is dominated by the Great Basin high over the southwestern United States. Modulated by upper level synoptic activity, it causes 3 to 6 days events of northwesterly winds (8-12 m s-1) directed along the gulf's axis, which are coherent over basin scales, and bring cool, dry desert air over the gulf. The vertical scale of these winds is 700-1000 m over land on the western side of the gulf, close to the height of the Baja California mountains, but only 100-400 m over water, defined by the wintertime inversion. Cross-gulf winds, related to topographic effects during upper level trough passages over Baja California, are particularly intense in the northwestern portion of the gulf. The winter marine layer is defined by a 1° to 4.5°C temperature inversion and a dew point temperature of 6°-11°C (a moisture content of 6-8 g kg-1); weak subsidence reduces dew point values to -4°C above the inversion. Winter winds above the marine layer are coherent (0.8) across the width of the gulf. The summer large-scale pressure field is dominated by a thermal low over the southwestern United States, and drives weak (2-5 m s-1) southeasterly winds, also directed primarily along the gulf, which are less spatially uniform than winter winds. Air temperature and moisture content are rather constant, and topographic effects are absent. The summer marine layer is on the order of 200-300 m thick, with dew point temperatures of 26°-28°C (21-24 g kg-1), and capped by a weak temperature inversion

  2. Tra corti e campi di battaglia: Alfonso d’Avalos, Luigi Tansillo e le affinità elettive tra petrarchisti napoletani e spagnoli

    Directory of Open Access Journals (Sweden)

    Tobia R. Toscano

    2012-06-01

    Full Text Available Tra tutte le capitali che entrarono a far parte del grande impero di Carlo V, Napoli appare, fin dal soggiorno di Garcilaso, il luogo ideale per l’esercizio della poesia lirica: qui era già molto sviluppato quel processo di compenetrazione tra armas y letras che costituisce la divisa di una nuova pleiade di petrarchisti, che, accanto alla occupazione prevalente del servizio militare, avevano sviluppato già sul declinare del sec. XV un interesse e una pratica costanti della poesia, anticipando nella prassi il modello del perfetto cortegiano, assunto poi a modello dalle élites spagnole. Figure di grande rilievo in questo processo di modellizzazione possono essere considerati Alfonso d’Avalos, marchese del Vasto, e Luigi Tansillo, i cui manoscritti di rime per il III Duca di Sessa ebbero grande diffusione in Spagna, incrociandosi con l'esperienza lirica di Gutierre de Cetina, che sulla scorta di Tansillo introdurrà nella poesia spagnola la forma metrica del madrigale, non trattata né da Garcilaso né da Boscàn.Parmi toutes les capitales qui firent partie du grand Empire de Charles-Quint, Naples semble, à partir du séjour de Garcilaso, le lieu idéal pour l’exercice de la poésie lyrique. Le mariage des armes et des lettres (armas y letras y était déjà très avancé et était devenu la devise d’une nouvelle pléiade de pétrarquistes. Leur intérêt pour la poésie leur avait fait développer dès la fin du XVe siècle, en marge de leur occupation principale, le service militaire, une constante pratique de la poésie, anticipant le modèle du parfait courtisan, que les élites espagnoles allaient imiter. Dans ce processus de modélisation, une place particulière revient à Alfonso d’Ávalos, marquis del Vasto, et à Luigi Tansillo, dont les manuscrits de poésies pour le IIIe duc de Sessa connurent une importante diffusion en Espagne, où ils croisèrent l’expérience lyrique de Gutierre de Cetina. Celui-ci, à la suite de

  3. Revisión del inventario y levantamiento de precisión de los puntos topográficos ubicados en el Campus Alfonso XIII de la UPCT

    OpenAIRE

    Tomás Ramírez de Arellano, Macarena

    2015-01-01

    El primer objetivo de este proyecto es el de disponer de un “inventario de puntos” situados en el campus Alfonso XIII, realizando para ello un levantamiento de precisión. Este nos debe permitir calcular las coordenadas planas (X, Y) de los mencionados puntos del campus con uno de los métodos topográficos especiales más precisos que podemos desarrollar, como es el caso del método de poligonación, o itinerario, realizado mediante “centrado forzado”. La coordenada Z se determinará mediante un le...

  4. Muerte y espacio artístico en el hombre colonizado: análisis de la novela corta "la piel" de Alfonso Hernández Catá.

    OpenAIRE

    Michelle María, Álvarez Amargós

    2012-01-01

    El espacio artístico y la muerte se constituyeron en grandes obsesiones que acompañaron los textos narrativos de Alfonso Hernández Catá. Las relaciones que se establecen entre estos dos elementos en la novela corta “La piel”, perteneciente a la colección Los frutos ácidos, resultan el objetivo del presente trabajo, el cual se realizará a partir de los presupuestos del método de análisis de contenido. Esta novela corta está basada en los prejuicios de la clase media y en el hombre que ha sido ...

  5. A Dynamic Gulf

    Institute of Scientific and Technical Information of China (English)

    2011-01-01

    The Pan-Beibu Gulf region will be the growth engine for China-ASEAN cooperation After running a travel company in Cambodia for more than a decade,Mo Chunrong decided to return to Nanning, capital of Guangxi Zhuang Autonomous Region,

  6. Long-Period Ground Motion in the Arabian Gulf from Earthquakes in the Zagros Mountains Thrust Belt

    Science.gov (United States)

    Pitarka, Arben; Al-Amri, Abdullah; Pasyanos, Michael E.; Rodgers, Arthur J.; Mellors, Robert J.

    2015-10-01

    The Arabian Gulf is adjacent to the Zagros Mountains, one of the most seismically active regions in the world. We observe that broadband seismic records of Zagros earthquakes recorded on the Arabian side of the Gulf display long-duration surface waves. While shorter periods (10 km) of the Gulf basin, the long-period energy is enhanced and transmitted efficiently. Consequently, large earthquakes in the Zagros could result in amplified ground motions at long periods (2-10 s) relative to average behavior. Such ground motions are of concern for large engineered structures, such as tall buildings and long bridges with resonant periods in the same period range. Here we present results of investigations of the characteristics of ground motions recorded on the western shore of the Gulf from selected earthquakes in the Zagros Mountains region. Exceptionally, long-duration seismic waves, as compared with standard models, are shown to occur with periods of 2-10 s. This may be due to waveguide effects in the deep sedimentary basin structure of the Arabian Platform. In addition to analyzing recorded ground motion we performed 3D wave propagation simulations using a finite difference method and experimental velocity models of the Gulf, with different shallow sedimentary layers structures. The simulation results confirm our hypothesis that long-period waves with extremely long duration and relatively large amplitudes are caused by the geometry of the basin sedimentary layers and, to some extent, by shallow earthquake depths. Combined effects of basin edge geometry with sharp velocity contrasts and shallow sources (<10 km) on the eastern side of the Arabian Gulf can cause large long-period ground motion on the western side of the Gulf. In contrast, the short-period content of ground motion (<2 s) at long distances is relatively weak. This is mainly due to wave propagation scattering and attenuation in the shallow sedimentary layers of the Gulf basin.

  7. Hurricane slams gulf operations

    International Nuclear Information System (INIS)

    This paper reports that reports of damage by Hurricane Andrew escalated last week as operators stepped up inspections of oil and gas installations in the Gulf of Mexico. By midweek, companies operating in the gulf and South Louisiana were beginning to agree that earlier assessments of damage only scratched the surface. Damage reports included scores of lost, toppled, or crippled platforms, pipeline ruptures, and oil slicks. By midweek the U.S. coast Guard had received reports of 79 oil spills. Even platforms capable of resuming production in some instances were begin curtailed because of damaged pipelines. Offshore service companies the another 2-4 weeks could be needed to fully assess Andrew's wrath. Lack of personnel and equipment was slowing damage assessment and repair

  8. Gulf operators resuming production

    International Nuclear Information System (INIS)

    This paper reports that Gulf of Mexico operators last week were gradually restoring production at installations struck by Hurricane Andrew. The Minerals Management Service continued receiving reports of more damage. By the end of the day Sept. 8, MMS had received reports of damage to 83 pipeline segments and 193 platforms and satellite installations. Damage reports listed 112 installations with structural damage, 13 platforms toppled and five leaning, and 30 satellite platforms toppled and 33 leaning. But despite the extent of damage the storm inflicted on oil and gas installations in the gulf, it pales in comparison to the misery and suffering the storm caused in Florida and Louisiana, an oil company official said

  9. Evolution and seismic expression of Mesozoic and Cenozoic shelf margins, Gulf of Mexico and vicinity

    Energy Technology Data Exchange (ETDEWEB)

    Buffler, R.T.

    1983-03-01

    Mapping and classification of modern and ancient shelf margins provide a basis for a concise post-rifting history of the Gulf of Mexico basin. Many hydrocarbon occurrences in the basin can be related to styles of shelf margins and their associated slope with implications for frontier exploration in deep-water facies. Seven basic types of shelf margins have been recognized and are discussed.

  10. Site characterization plan: Gulf Coast salt domes

    International Nuclear Information System (INIS)

    The National Waste Terminal Storage (NWTS) program of the US Department of Energy (DOE) is responsible for developing technology and providing facilities for safe, environmentally acceptable, permanent disposal of high-level nuclear waste. The Office of Nuclear Waste Isolation has been intensively investigating Gulf Coast Salt Dome Basin salt domes and bedded salt in Texas and Utah since 1978. In the Gulf Coast, the application of screening criteria in the region phase led to selection of eight domes for further study in the location phase. Further screening in the area phase identified four domes for more intensive study in the location phase: Oakwood Dome, Texas; Vacherie Dome, Louisiana; and Richton Dome and Cypress Creek Dome, Mississippi. For each dome, this Site Characterization Plan identifies specific hydrologic, geologic, tectonic, geochemical, and environmental key issues that are related to the DOE/NWTS screening criteria or affect the feasibility of constructing an exploratory shaft. The Site Characterization Plan outlines studies need to: (1) resolve issues sufficiently to allow one or more salt domes to be selected and compared to bedded salt sites in order to determine a prime salt site for an exploratory shaft; (2) conduct issue-related studies to provide a higher level of confidence that the preferred salt dome site is viable for construction of an exploratory shaft; and (3) provide a vehicle for state input to issues. Extensive references, 7 figures, 20 tables

  11. Status of Gulf Coast salt dome characterization

    International Nuclear Information System (INIS)

    Screening and characterization for a potential nuclear waste repository have progressed through the area phase in these Gulf Coast Salt Basins. The domes studied during the area phase are described briefly. The area characterization studies are outlined, and the resulting reports are listed. Geologic and environmental studies resulted in elimination of four domes from further consideration. The remaining domes were judged acceptable and were classified as to their favorability to license. Site characterization planning for location phase activities deals primarily with technical, environmental, and socioeconomic issues of concern to the states and/or to the Office of Nuclear Waste Isolation (ONWI), Department of Energy (DOE). These issues are listed and discussed. 16 references, 9 figures

  12. Thermocline Regulated Seasonal Evolution of Surface Chlorophyll in the Gulf of Aden

    KAUST Repository

    Hoteit, Ibrahim

    2015-04-01

    The Gulf of Aden, although subject to seasonally reversing monsoonal winds, has been previously reported as an oligotrophic basin during summer, with elevated chlorophyll concentrations only occurring during winter due to convective mixing. However, the Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) ocean color data reveal that the Gulf of Aden also exhibits a prominent summer chlorophyll bloom and sustains elevated chlorophyll concentrations throughout the fall, and is a biophysical province distinct from the adjacent Arabian Sea. Climatological hydrographic data suggest that the thermocline, hence the nutricline, in the entire gulf is markedly shoaled by the southwest monsoon during summer and fall. Under this condition, cyclonic eddies in the gulf can effectively pump deep nutrients to the surface layer and lead to the chlorophyll bloom in late summer, and, after the transition to the northeast monsoon in fall, coastal upwelling driven by the northeasterly winds produces a pronounced increase in surface chlorophyll concentrations along the Somali coast.

  13. Fish larval transport in a macro-tidal regime: Gulf of Kachchh, west coast of India

    Digital Repository Service at National Institute of Oceanography (India)

    George, G.; Vethamony, P.; Sudheesh, K.; Babu, M.T.

    This study combines observational data with a two-dimensional numerical model results to determine the fate of fish eggs released in the Gulf of Kachchh (GoK), a semi enclosed basin on the west coast of India. Fish eggs were treated as passive...

  14. Hurricane shuts down gulf activity

    International Nuclear Information System (INIS)

    This paper reports that producers in the Gulf of Mexico and plant operators in South Louisiana last week were checking for damage wrought by Hurricane Andrew. In its wake Andrew left evacuated rigs and platforms in the gulf and shuttered plants across a wide swath of the Gulf Coast. Operations were beginning to return to normal late last week. Not all gulf operators, especially in the central gulf, expected to return to offshore facilities. And even producers able to book helicopters did not expect to be able to fully assess damage to all offshore installations before the weekend. MMS officials in Washington estimated that 37,500 offshore workers were evacuated from 700 oil and gas installations on the gulf's Outer Continental Shelf. Gulf oil and gas wells account for about 800,000 b/d of oil and one fourth of total U.S. gas production. MMS was awaiting an assessment of hurricane damage before estimating how soon and how much gulf oil and gas production would be restored

  15. Influence of resonance on tide and storm surge in the Gulf of Thailand

    Science.gov (United States)

    Tomkratoke, Saifhon; Sirisup, Sirod; Udomchoke, Veerasak; Kanasut, Jirawat

    2015-10-01

    A numerical simulation is used to determine the effective resonance period, quality factor Q and linear friction coefficient and mechanism of tide and storm surge in the Gulf of Thailand. The results indicated that the resonance response is triggered by the forced wave with the period of 20.25 hours. The Q factor and linear friction coefficient are approximately 3.15 and 2.76×10-5 ms-1, respectively. The gulf is regarded as a moderately dissipative system, which may yield small amplification for the oscillating forced wave. The resonance structure of the basin can play an important role in spatial distribution and amplification of tidal waves in the Gulf of Thailand and nearby area. Distance from the effective resonance period and the corresponding Q factor can be employed in characterizing of tidal amplification in the gulf. The study found that phase difference in the incoming tidal waves can induce the distortion of a nodal band to the normal mode analysis results. The resonance in the north-south direction is the principal mechanism to control tidal waves, specifically for the upper part of the gulf (the Gulf of Thailand). However, significant effect of resonance in the west-east direction on the amplification of tidal waves near the southern part of the gulf (Vietnam, Malaysia and Singapore coast) may be pronounced. From the reproduced historic storm surge and hypothetical results, the spatial distribution of storm surge elevation and the response ratio are in good agreement with the resonance mode and Q factor of the basin. Individually, the contribution of resonance factor to induce severe storm surge (positive surge) tends to be insignificant. Conversely, the interaction process between the disturbance system and the propagating surge wave in the gulf can induce large positive surge near the landfall location significantly.

  16. WATER TEMPERATURE, SALINITY, and HYDROSTATIC PRESSURE collected from R/V Point Sur in Entrance to the Gulf of California from 2013-04-19 to 2013-05-02 (NCEI Accession 0131072)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Hydrographic data were collected in Pescadero Basin (at the entrance to the Gulf of California) and subsequently along the West Coast of Baja California and...

  17. Clay Mineral Distribution Patterns of Tertiary Continental Oil-bearing Basins in China

    Institute of Scientific and Technical Information of China (English)

    Zhao Xingyuan

    1996-01-01

    @@ Induction This paper studies the clay mineral distribution patterns of Tertiary continental oil-bearing basins in China. More than 9 000 shale samples from Paleogene (E) to Neogene (N) Series distributed in Bohai Gulf, Subei, Jianghan,Nanxiang, Zhoukou, Sanshui, Beibu Bay, East China Sea,Hetao, Juiquan, Qaidam and Tarim basins, and so on.

  18. Bibliography, geophysical data locations, and well core listings for the Mississippi Interior Salt Basin

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1998-05-01

    To date, comprehensive basin analysis and petroleum system modeling studies have not been performed on any of the basins in the northeastern Gulf of Mexico. Of these basins, the Mississippi Interior Salt Basin has been selected for study because it is the most petroliferous basin in the northeastern Gulf of Mexico, small- and medium-size companies are drilling the majority of the exploration wells. These companies do not have the resources to perform basin analysis or petroleum system modeling research studies nor do they have the resources to undertake elaborate information searches through the volumes of publicly available data at the universities, geological surveys, and regulatory agencies in the region. The Advanced Geologic Basin Analysis Program of the US Department of Energy provides an avenue for studying and evaluating sedimentary basins. This program is designed to improve the efficiency of the discovery of the nation`s remaining undiscovered oil resources by providing improved access to information available in the public domain and by increasing the amount of public information on domestic basins. This report provides the information obtained from Year 1 of this study of the Mississippi Interior Salt Basin. The work during Year 1 focused on inventorying the data files and records of the major information repositories in the northeastern Gulf of Mexico and making these inventories easily accessible in an electronic format.

  19. Geological evaluation of Gulf Coast salt domes: overall assessment of the Gulf Interior Region

    International Nuclear Information System (INIS)

    The three major phases in site characterization and selection are regional studies, area studies, and location studies. This report characterizes regional geologic aspects of the Gulf Coast salt dome basins. It includes general information from published sources on the regional geology; the tectonic, domal, and hydrologic stability; and a brief description the salt domes to be investigated. After a screening exercise, eight domes were chosen for further characterization: Keechi, Oakwood, and Palestine Domes in Texas; Vacherie and Rayburn's domes in North Louisiana; and Cypress Creek and Richton domes in Mississippi. A general description of each, maps of the location, property ownership, and surface geology, and a geologic cross section were presented for each dome

  20. Geological evaluation of Gulf Coast salt domes: overall assessment of the Gulf Interior Region

    Energy Technology Data Exchange (ETDEWEB)

    None

    1981-10-01

    The three major phases in site characterization and selection are regional studies, area studies, and location studies. This report characterizes regional geologic aspects of the Gulf Coast salt dome basins. It includes general information from published sources on the regional geology; the tectonic, domal, and hydrologic stability; and a brief description the salt domes to be investigated. After a screening exercise, eight domes were chosen for further characterization: Keechi, Oakwood, and Palestine Domes in Texas; Vacherie and Rayburn's domes in North Louisiana; and Cypress Creek and Richton domes in Mississippi. A general description of each, maps of the location, property ownership, and surface geology, and a geologic cross section were presented for each dome.

  1. Reflection seismic studies in the macrotidal Gulf of Kachchh, India: Evidence of physiographic evolution

    Digital Repository Service at National Institute of Oceanography (India)

    Chauhan, O.S.; Vora, K.H.

    ) Investigations and studies for tidal power development in the Gulf of Kachchh. Interim Report, Central Electricity Authority, India, 250 pp. 396 o.s. CHAUnAN and K. H. Vo~ BISWAS S. K. (1982) Rift basins in western margins of India and their hydrocarbon... Research, Vol. 10. No. 4, pp. 385-396. 1990. 0278-4343/90 $3.00 + 0.00 Printed in Great Britain. (~) 1990 Pergamon Press plc NOTE Reflection seismic studies in the macrotidal Gulf of Kachchh, India: evidence of physiographic evolution O. S. CHAUHAN...

  2. Distribution and ecology of deep-water benthic foraminifera in the Gulf of Mexico

    Science.gov (United States)

    Poag, C.W.

    1984-01-01

    Bathyal and abyssal foraminifera in the Gulf of Mexico are distributed among thirteen generic predominance facies. Five predominance facies nearly encircle the Gulf basin along the slope and rise; a sixth predominance facies blankets the Sigsbee Plain, and a seventh is restricted to the Mississippi Fan. The remaining eight predominance facies have more restricted distributions. The areal patterns of these predominance facies can be related chiefly to water mass and substrate characteristics; modifications are brought about by calcite dissolution, upwelling, and sill depth. Analysis of ancient generic predominance facies is useful in predicting relative paleobathymetry and other paleoenvironmental properties. ?? 1984.

  3. Erosional processes and paleo-environmental changes in the Western Gulf of Lions (SW France) during the Messinian Salinity Crisis

    OpenAIRE

    Lofi, Johanna; Gorini, Christian; Berne, Serge; Clauzon, Georges; Dos Reis, A.tadeu; Ryan, William; Steckler, Michael

    2005-01-01

    Current interpretation of the Messinian Salinity Crisis (MSC) involves partial "clesiccation" of the Mediterranean Sea coupled with the deposition of thick evaporites in the deep basins. New sets of seismic reflection profiles in the western part of the Gulf of Lions confirm the basinward extension of the Messinian erosion and enable the mapping of distinctive seismic markers indicating the Messinian Erosional Surface (or Messinian unconformity), the basin-margin detrital deposits, and the de...

  4. Convective upwelling in the mantle beneath the Gulf of California.

    Science.gov (United States)

    Wang, Yun; Forsyth, Donald W; Savage, Brian

    2009-11-26

    In the past six million years, Baja California has rifted obliquely apart from North America, opening up the Gulf of California. Between transform faults, seafloor spreading and rifting is well established in several basins. Other than hotspot-dominated Iceland, the Gulf of California is the only part of the world's seafloor-spreading system that has been surrounded by enough seismometers to provide horizontal resolution of upper-mantle structure at a scale of 100 kilometres over a distance great enough to include several spreading segments. Such resolution is needed to address the long-standing debate about the relative importance of dynamic and passive upwelling in the shallow mantle beneath spreading centres. Here we use Rayleigh-wave tomography to image the shear velocity in the upper 200 kilometres or so of the mantle. Low shear velocities similar to those beneath the East Pacific Rise oceanic spreading centre underlie the entire length of the Gulf, but there are three concentrated locations of anomalously low velocities spaced about 250 kilometres apart. These anomalies are 40 to 90 kilometres beneath the surface, at which depths petrological studies indicate that extensive melting of passively upwelling mantle should begin. We interpret these seismic velocity anomalies as indicating that partial melting triggers dynamic upwelling driven by either the buoyancy of retained melt or by the reduced density of depleted mantle. PMID:19940924

  5. Gulf Petro Initiative

    Energy Technology Data Exchange (ETDEWEB)

    Fathi Boukadi

    2011-02-05

    In this report, technologies for petroleum production and exploration enhancement in deepwater and mature fields are developed through basic and applied research by: (1) Designing new fluids to efficiently drill deepwater wells that can not be cost-effectively drilled with current technologies. The new fluids will be heavy liquid foams that have low-density at shallow dept to avoid formation breakdown and high density at drilling depth to control formation pressure. The goal of this project is to provide industry with formulations of new fluids for reducing casing programs and thus well construction cost in deepwater development. (2) Studying the effects of flue gas/CO{sub 2} huff n puff on incremental oil recovery in Louisiana oilfields bearing light oil. An artificial neural network (ANN) model will be developed and used to map recovery efficiencies for candidate reservoirs in Louisiana. (3) Arriving at a quantitative understanding for the three-dimensional controlled-source electromagnetic (CSEM) geophysical response of typical Gulf of Mexico hydrocarbon reservoirs. We will seek to make available tools for the qualitative, rapid interpretation of marine CSEM signatures, and tools for efficient, three-dimensional subsurface conductivity modeling.

  6. Physical Oceanography of the Gulf of Aden

    Digital Repository Service at National Institute of Oceanography (India)

    Al Saafani, M.A.

    was generally weak with an anticyclonic eddy in the eastern gulf. During August, an anticyclonic eddy appeared in the center of the gulf and another near the eastern end of the gulf between 50 ◦ E and 52 ◦ E. Murray and Johns [1997] studied the exchange between...

  7. La dialéctica texto-imagen. A propósito de la representación del judío en las “Cantigas de Santa María” de Alfonso X

    Directory of Open Access Journals (Sweden)

    Rodríguez Barral, Paulino

    2007-06-01

    Full Text Available The treatment of the image of Jews in the Cantigas by Alfonso X fluctuates between their total condemnation and the perspective of salvation. The condemnation of Judaism embodies some classic topics of medieval anti-Semitism such as alliance with the devil, infanticide, ritual murder, or sacrilegious desecration. This negative vision is tempered in some cantigas in which their jewish protagonists embrace the Christian faith as a result of Virgin Mary's intervention.

    This ambiguity may be a reflection of the monarch's attitude towards Judaism. On the one hand his reign is marked by prejudice both in certain proceedings and in the regulations of the Partidas, but on the other some Jews cooperate actively with the king's cultural and and scientific undertakings and even hold important public positions.



    El tratamiento de la imagen del judío en las Cantigas de Alfonso X oscila entre la condena sin paliativos y la perspectiva de la salvación. La primera toma cuerpo en algunos de los motivos clásicos del antisemitismo medieval como la alianza con el diablo, el infanticidio, el crimen ritual, o la profanación sacrílega. Una visión extremadamente negativa que se matiza en aquéllas cantigas en las que sus protagonistas, a instancias de la intervención mariana, acaban abrazando la fe cristiana.

    Probablemente haya que ver en todo ello un reflejo de la ambigüedad que, en relación al judaísmo, caracteriza el

  8. La financiación de las empresas mediterráneas de Alfonso el Magnánimo. Bailía General, Subsidios de Cortes y Crédito Institucional en Valencia (1419-1455

    Directory of Open Access Journals (Sweden)

    Mira Jódar, Antonio José

    2003-12-01

    Full Text Available This article studies the role of the General Bailía of Valencia—the office for the management of the royal domain resources of the kingdom of Valencia- in the political and military projects of Alfonso V the Magnanimous in the Mediterranean. In this way its also analysed the role of the Parliament, a class representation of the kingdom, and the city of Valencia, main urban centre The incomes from the royal domain, the donations from the Parliaments as a representative assemblies, and the loans provided by the city of Valencia contributed in a decisive way to the guarantee of the economic viability of Alfonso Vs military expansion. It is right that the main instruments that the king had to apply his aggressive policy was, on the one hand, the centralized and complex organization around the General Treasure of the Crown of Aragon and, later on, to the Treasure of the Kingdom of Naples; on the other hand, to the solid banking infrastructure built around the Mediterranean. Therefore, both of them were based on the confidence and guaranties offered by the powerful ordinary and non ordinary tax structures of the kingdom, and the solid financial support given by the institutions of the kingdom.

    En este trabajo se pretende determinar la funciones respectivas que la bailía general de Valencia, como oficina administradora de los recursos patrimoniales de la corona, las Cortes, en su calidad de representación estamental del reino, y la ciudad de Valencia, el principal centro urbano del país, desempeñaron en la financiación de los ambiciosos proyectos político-militares de Alfonso V en el Mediterráneo. De hecho, las rentas derivadas del Real Patrimonio, los donativos proporcionados por las asambleas representativas y los préstamos facilitados por el municipio contribuyeron decisivamente a garantizar la viabilidad económica de las empresas bélicas del Magnánimo. Es cierto que los principales instrumentos con los que contaba el monarca

  9. Analysis of Temporal Variability of Measured and Modeled Vertical Distributions of Salinity and Temperature in the Gulf of Finland during 10-Year Period

    OpenAIRE

    PASSENKO Jelena; LESSIN GENNADI; Raudsepp, Urmas; Maljutenko, Ilja; Neumann, Thomas; Laanemets, Jaan

    2010-01-01

    The Gulf of Finland is the sub-basin of the Baltic Sea seriously affected by eutrophication. General Estuarine Transport Model (GETM) was used for modeling hydrophysical fields of the Gulf during the period from 1997 to 2005. The results of the hydrodynamic modeling are important input for ecosystem modeling, in which salinity and temperature variations play the most important role. An accurately simulated salinity field is to some extent a proof that the transport of passive bio-chemical tra...

  10. GIS Plate Tectonic Reconstruction of the Gulf of California-Salton Trough Oblique Rift

    Science.gov (United States)

    Skinner, L. A.; Bennett, S. E.; Umhoefer, P. J.; Oskin, M. E.; Dorsey, R. J.; Nava, R. A.

    2011-12-01

    We present GIS-based plate tectonic reconstruction maps for the Gulf of California-Salton Trough oblique rift. The maps track plate boundary deformation in 2 and 1 Myr slices (6-2 Ma and 2 Ma-present) using a custom ArcGIS add-in tool to close extensional basins and restore slip on dextral faults. The tool takes a set of polygons depicting present day locations of tectonic blocks and sequentially restores displacement of their centroids along a vector specific to that time slice. Tectonic blocks are defined by faults, geology, seismic data, and bathymetry/topography. Spreading center and fault-slip rates were acquired from geologic data, cross-Gulf tie points, GPS studies, and aeromagnetic data. A recent GPS study indicated that ~92% of modern-day Pacific-North America (PAC-NAM) plate motion is localized between the Baja California microplate and North America. Relative plate motion azimuth varies from ~302° in the southern Gulf to ~314° in the Salton Trough. Baja-North America GPS rates agree remarkably with ~6 Ma geologic offsets across the Gulf and are used during reconstruction steps back to 6 Ma. In the southern Gulf, unpublished GPS data indicate that modern plate motion is partitioned between the plate boundary, Gulf-margin system, and borderland faults west of Baja California. The Alarcon and Guaymas spreading centers initiated at 2.4 Ma and 6 Ma (Lizarralde et al., 2007), respectively, while the Farallon, Pescadero, and Carmen spreading centers began between ~2-1 Ma (Lonsdale, 1989). Therefore, the 2, 4, and 6 Ma reconstruction steps include a long transtensional fault zone along much of the southern Gulf, connecting the Guaymas spreading center with either the Alarcon spreading center or East Pacific Rise. In the northern Gulf, transtensional strain initiated in coastal Sonora by ~7 Ma and migrated westward as the Gulf opened. At ~6 Ma strain migrated west into marine pull-apart basins that now lie within the eastern Gulf. Seismic reflection studies

  11. Distribution, habitat use and ecology of deepwater Anemones (Actiniaria) in the Gulf of Mexico

    Science.gov (United States)

    Ammons, Archie W.; Daly, Marymegan

    2008-12-01

    The distribution of deepwater Actiniaria is poorly known. Rarely are these organisms identified to family, as this requires both well-preserved specimens and taxonomic expertise. Ecological information is similarly lacking. From the results of a comprehensive surveying program in the deep Gulf of Mexico, we report the occurrence of nine species of Actiniaria. For the most abundant four of these, we plot distributions and discuss habitat use, morphological variation, and feeding strategies. Actiniaria in the Gulf appear to have broad, basin-wide distributions with little depth preference. Faunal biomass is highest in the NE Gulf within submarine canyons or at the base of slope escarpments. Attachment mode is mostly opportunistic on various types of hard substrata, including trash. Sediment-dwelling forms are very abundant at an organically rich site within a large submarine canyon.

  12. Coastal change and hypoxia in the northern Gulf of Mexico: Part I

    Directory of Open Access Journals (Sweden)

    2007-01-01

    Full Text Available The Committee on Environment and Natural Resources (CENR has identified the input of nutrient-rich water from the Mississippi/Atchafalaya River Basin (MARB as the prime cause of hypoxia in the northern Gulf of Mexico and the prime means for its control. A Watershed Nutrient Task Force was formed to solve the hypoxia problem by managing the MARB catchment. However, the hypoxic zone is also experiencing massive physical, hydrological, chemical and biological changes associated with an immense river-switching and delta-building event that occurs here about once a millennium. Coastal change induced hypoxia in the northern Gulf of Mexico prior to European settlement. It is recommended that for further understanding and control of Gulf hypoxia the Watershed Nutrient Task Force adopt a truly holistic environmental approach which includes the full effects of this highly dynamic coastal area.

  13. Too many eggs in one basket? US Gulf coast and Gulf of Mexico risks not just technical

    International Nuclear Information System (INIS)

    The reasons behind the waning gas supply in North America were discussed. Gas prices in North America are currently 3 times higher than they were in 1990. Although there are twice as many rigs, drilling twice as many wells, 5 to 20 per cent deeper, they are finding one third less recoverable gas than in 1990. It was emphasized that the continental gas supply system is vulnerable to upsets in much the same way that the global surplus oil production capacity was affected by upsets. North America has relied on 2 major basins to supply two thirds of its gas. These include the Western Canada Sedimentary Basin as well as the region encompassing the Gulf of Mexico, southern Texas and Louisiana. Both major basins are in rapid decline. In addition, hurricanes in the Gulf of Mexico have increased in both intensity and frequency, ensuing damage to oil and gas infrastructure and dislocating the continent's gas system. This trend is expected to continue and the periodic advisory reports from the National Petroleum Council indicate an austere future for gas supply and demand, with a reliance on difficult, remote, uncertain and costly supplies. The economy, energy consumption, storage, supply and weather are all factors that contribute to the rising gas prices in North America. The author claimed that North American gas supply has been and continues to be constrained by misguided policies. Given the decline in the main supply basins, gas supply is expected to remain tight barring weaker gross domestic product (GDP). It was emphasized that weather-dominated North American gas markets will increasingly affect the rest of the world, including Europe which has its own gas supply concerns and which is increasingly linked to North America's gas supply problem. figs

  14. Gramíneas uruguayas de D. José Arechavaleta (1838-1912, en el Real Colegio Alfonso XII de San Lorenzo de El Escorial (Madrid, España

    Directory of Open Access Journals (Sweden)

    Carrasco, María A.

    2001-12-01

    Full Text Available The Royal Monastery of El Escorial was built in the xvi century by king Felipe U. In the part intended to be a college and seminary, the Real Colegio Alfonso XII was established in 1885. In this place, the treasures that had been accumulated for fíve hundred years, that carne from acquisitions, collections and donations, are stored. In this paper we present a small collection, of undeniable historical valué. It contains 186 Gramineae that were sent as a present to María Cristina, the Regent Queen of Spain, by the President of Uruguay on the occasion of the World Exhibition of Barcelona in 1888. The plants are part of the herbarium of the Flora Uruguaya of José Arechavaleta y Balparda [Santurce (España, 1838-Montevideo (Uruguay, 1912]. Some of the plants are annotated by Arechavaleta as new species, and some belong from the loc. clas. All this material is identified by Arechavaleta and J. Hackel.El Real Monasterio de El Escorial fue fundado en el siglo XVI por el rey Felipe n. En la parte dedicada a colegio-seminario se estableció en 1885 el Real Colegio Alfonso XII, donde están depositados todos los fondos que se han ido acumulando a lo largo de quinientos años, procedentes de adquisiciones, recolecciones y donaciones. En este trabajo presentamos una colección, pequeña pero de indudable valor histórico, de 186 Gramineae que fueron enviadas por el presidente del Uruguay a la reina regente de España con motivo de la Exposición Universal de Barcelona celebrada en 1888. Estos materiales son parte del herbario de la Flora Uruguaya de D. José Arechavaleta y Balparda [Santurce (España, 1838-Montevideo (Uruguay, 1912]. Algunas plantas están anotadas por Arechavaleta como especies nuevas -unas cuantas proceden de la localidad clásica- y todas ellas están identificadas por Arechavaleta o J. Hackel.

  15. Facing Today's Exploration Challenges in the Gulf of Mexico

    Science.gov (United States)

    Detomo, R.

    2005-05-01

    The Gulf of Mexico represents one of the most intensively explored basins in the world, and yet it still delivers significant new material oil and gas discoveries every year. Because of it high productivity, geologic complexity, competitive acreage access and large profitability margins, the Gulf of Mexico presents many industry-leading challenges to Exploration today. For major companies exploring for oil and gas in the Gulf of Mexico today, their challenge is to "safely, responsibly and profitably find and produce reduced accumulations in increasingly hostile settings." The GoM serves as the sportsman's playground for a significant population located in and around its waters, and therefore, operating safely and responsibly are unassailable moral and operational standards by which we sustain future development, and maintain our license to operate. With that as a backdrop, today's challenges are driven by the nature of where the business is looking for new reserves in this extremely mature basin. These "Opportunities" encompass the following: 1) large, under-explored, sub-salt areas, characterized by poor seismic imaging, uncertain geologic regimes and potentially dangerous overpressures, 2) deep true-vertical-depth opportunities in older rocks that challenge our understanding of reservoir quality prediction and hydrocarbon systems, and are at the edge of today's drilling technologies, 3) access to sensitive areas including the eastern GoM-Florida shelf, coastal areas and international borders, 4) challenging "small accumulation" discoveries that cannot support expensive appraisal or development options, are remote to infrastructure or inefficiently produce the reservoir, and finally 5) new play development, which is challenged by long maturation cycles, small acreage blocks, intense international competition, and rapid lease rolls. This talk will consider what Shell and the Oil & Gas Industry does today to succeed in this arena, and specifically will show examples

  16. Gulf and Dilmun Type seals

    DEFF Research Database (Denmark)

    Laursen, Steffen

    2011-01-01

    From around 2100 BC a glyptic tradition emerges in the Arabian Gulf, which is dependant on the well-established schools of the Indus Valley seal cutters. These circular hybrids of classic Harappan seals rapidly became popular amongst the merchants of Dilmun, centered on Bahrain Island. At first...... these Gulf Type‘ seals drew heavily on Indus Valley iconography and Indus script was occasionally employed in a pidgin-like manner. While the earliest circular seals incorporate features from Mesopotamian glyptic only to a lesser extent, this becomes a more important source of inspiration for later...

  17. The Role of Rift Obliquity in Formation of the Gulf of California

    Science.gov (United States)

    Bennett, Scott Edmund Kelsey

    The Gulf of California illustrates how highly oblique rift geometries, where transform faults are kinematically linked to large-offset normal faults in adjacent pull-apart basins, enhance the ability of continental lithosphere to rupture and, ultimately, hasten the formation of new oceanic basins. The Gulf of California rift has accommodated oblique divergence of the Pacific and North America tectonic plates in northwestern Mexico since Miocene time. Due to its infancy, the rifted margins of the Gulf of California preserve a rare onshore record of early continental break-up processes from which to investigate the role of rift obliquity in strain localization. Using new high-precision paleomagnetic vectors from tectonically stable sites in north-central Baja California, I compile a paleomagnetic transect of Miocene ignimbrites across northern Baja California and Sonora that reveals the timing and distribution of dextral shear associated with inception of this oblique rift. I integrate detailed geologic mapping, basin analysis, and geochronology of pre-rift and syn-rift volcanic units to determine the timing of fault activity on Isla Tiburon, a proximal onshore exposure of the rifted North America margin, adjacent to the axis of the Gulf of California. The onset of strike-slip faulting on Isla Tiburon, ca. 8 - 7 Ma, was synchronous with the onset of transform faulting along a significant length of the nascent plate boundary within the rift. This tectonic transition coincides with a clockwise azimuthal shift in Pacific-North America relative motion that increased rift obliquity. I constrain the earliest marine conditions on southwest Isla Tiburon to ca. 6.4 - 6.0 Ma, coincident with a regional latest Miocene marine incursion in the northern proto-Gulf of California. This event likely flooded a narrow, incipient topographic depression along a ˜650 km-long portion of the latest Miocene plate boundary and corresponds in time and space with formation of a newly

  18. 1400 yr multiproxy record of climate variability from the northern Gulf of Mexico

    Science.gov (United States)

    Richey, J.N.; Poore, R.Z.; Flower, B.P.; Quinn, T.M.

    2007-01-01

    A continuous decadal-scale resolution record of climate variability over the past 1400 yr in the northern Gulf of Mexico was constructed from a box core recovered in the Pigmy Basin, northern Gulf of Mexico. Proxies include paired analyses of Mg/Ca and δ18O in the white variety of the planktic foraminifer Globigerinoides ruber and relative abundance variations of G. sacculifer in the foraminifer assemblages. Two multi-decadal intervals of sustained high Mg/Ca indicate that Gulf of Mexico sea surface temperatures (SSTs) were as warm or warmer than near-modern conditions between 1000 and 1400 yr B.P. Foraminiferal Mg/Ca during the coolest interval of the Little Ice Age (ca. 250 yr B.P.) indicate that SST was 2–2.5 °C below modern SST. Four minima in the Mg/Ca record between 900 and 250 yr B.P. correspond with the Maunder, Spörer, Wolf, and Oort sunspot minima, suggesting a link between changes in solar insolation and SST variability in the Gulf of Mexico. An abrupt shift recorded in both δ18Ocalcite and relative abundance of G. sacculifer occurred ca. 600 yr B.P. The shift in the Pigmy Basin record corresponds with a shift in the sea-salt-sodium (ssNa) record from the Greenland Ice Sheet Project 2 ice core, linking changes in high-latitude atmospheric circulation with the subtropical Atlantic Ocean.

  19. Seismic stratigraphy and geologic history of Jurassic rocks, northeastern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Dobson, L.M.; Buffler, R.T. [Univ. of Texas, Austin, TX (United States)

    1997-01-01

    A grid of two-dimensional seismic data tied to exploration wells defines four Jurassic sequences in the northeastern Gulf of Mexico. These sequences correlate with well-known northern Gulf of Mexico basin stratigraphic units: the Louann Salt (L sequence), Norphlet and Smackover formations (N-S sequence), Haynesville Formation (H sequence), and Cotton Valley Group (C sequence). The Jurassic section overlies a basement surface characterized by broad highs (Middle Ground arch and Southern platform) and lows (Apalachicola basin and Tampa embayment). This basement structure controlled the distribution, thickness, and paleogeography of all the Jurassic sequences, but its influence became progressively less pronounced as sediment filled the basin. The Jurassic geologic history of the region is developed from an interpretation of these sequences. Well control documents the presence of Louann Salt in the Apalachicola basin, whereas in the Tampa embayment the interval is interpreted only from seismic data. Salt movement on the West Florida Shelf began early, during Norphlet-Smackover deposition, and slowed dramatically by the end of Haynesville deposition. Smackover paleogeography includes progradation of a carbonate shelf in the Apalachicola basin and the Tampa embayment, as well as development of carbonate buildups updip of basement hingelines, over basement highs, and above early salt structures. In the Apalachicola basin, Haynesville clastic sedimentation updip was coeval with carbonate deposition downdip, and a localized carbonate shelf margin developed to the southwest. Haynesville clastic sedimentation may have prevailed in the Tampa embayment, where oblique clinoforms represent shelf margin progradation. During deposition of the Cotton Valley sequence, the northeastern Gulf of Mexico was characterized by delta-plain and delta-platform sedimentation with seismically defined shelf margin progradation only in the Tampa embayment.

  20. Seismic stratigraphy of northern Green Canyon area, Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Mann, R.G.; Bryant, W.R.

    1986-05-01

    The Green Canyon area of the Gulf of Mexico is an active frontier exploration area of the continental slope underlain by relatively shallow salt or shale diapirs and ridges forming large intraslope basins and troughs. Analysis of more than 200 multichannel seismic profiles in this area show several seismic sequences within each basin or trough. The depositional history of the area is interpreted from the seismic sequences and seismic facies distribution within each basin. These facies are based on reflection configuration and include parallel to subparallel reflections, prograding clinoforms, hummocky clinoforms, chaotic zones, and acoustically semitransparent zones. Sigmoid and oblique progradational clinoforms are found at the shelf edge where outbuilding and aggradation occur. Hummocky clinoforms are widespread in each basin and occur in thick sequences. These grade vertically and laterally into parallel or semitransparent zones resulting in alternating reflection patterns. The parallel reflections can be interpreted as low-energy turbidites deposited during lower sea level. Chaotic zones show contorted stratal surfaces suggesting mass movement deposits. The evolution of each basin is unique. Structure and isopach maps of each sequence along with the facies distribution indicate several depositional mechanisms. These are possibly related to sea level fluctuations and shifting sediment supply. Correlation of sequences between basins and troughs is hampered in the western half of the area because of the presence of shallow subsurface diapirs and ridges, and large growth faults, and the absence of well data. Diapirs in the eastern half are less numerous and more isolated, with thicker sedimentary troughs between them because of the eastward migration of the Mississippi fan across this area in the Pliocene and Pleistocene.

  1. Messinian evaporite deposition during sea level rise in the Gulf of Lions (Western Mediterranean)

    OpenAIRE

    Bache, François; Gargani, Julien; Suc, Jean-Pierre; Gorini, Christian; Rabineau, Marina; Popescu, Speranta-Maria; Leroux, Estelle; Do Couto, Damien; Rubino, Jean-Loup; Olivet, Jean-Louis; Clauzon, Georges; Dos Reis, Antonio Tadeu; Aslanian, Daniel

    2015-01-01

    International audience The Messinian Salinity Crisis resulted from desiccation of the Mediterranean Sea after its isolation from the Atlantic Ocean at the end of the Miocene. Stratal geometry tied to borehole data in the Gulf of Lions show that the pre-crisis continental shelf has been eroded during a major sea-level fall and that sedi-ments from this erosion have been deposited in the basin. This detrital package is onlapped by high amplitude seismic reflectors overlain by the "Messinian ...

  2. Se nas pedras faz feguras parecer... Consideraciones sobre iconografía mariana y figuras poéticas en las Cantigas de Santa María de Alfonso X

    Directory of Open Access Journals (Sweden)

    Santiago Disalvo

    2014-12-01

    Full Text Available Marian iconography has been reflected in medieval Hispanic poetry in many ways, ranging from verses that describe the Virgin and her attributes to theological and mariological concepts expressed plastically by means of rhetorical forms. For example, the garden and the flowers as Holy Mary’s personal ornaments and symbols, or the image of light through a crystal or a glass window in the scenes of the Annunciation –with rich pictorial evidence throughout medieval art–, are present in poetry as symbolic descriptions of various extensions and genre, and, on the other hand, as Marian advocations or mariological tópoi as well (Ave/Eva, Flos, Hortus, Radix-Virga, Regina, Stella. Therefore, this paper proposes a general survey and a comparitive study on some of these procedures, focusing on King Alfonso X’s Cantigas de Santa Maria. In this sense, rhetorical figures, as tools that bridge the gap between the pictorial and the poetic, lead the reading towards a symbolic interpretation provided by the figuration or typologia, as postulated by Erich Auerbach for medieval textuality. Ultimately, the sacred value of Marian images (an inheritance of Byzantine iconic art is represented also in the miracles of the Cantigas de Santa Maria, a masterpiece that shows a strong influence of the iconodulic doctrine.

  3. The U.S. Geological Survey`s National Coal Resource Assessment: The Northern and Central Appalachian Basin

    Energy Technology Data Exchange (ETDEWEB)

    Ruppert, L.; Bragg, L.; Tewalt, S. [Geological Survey, Reston, VA (United States)

    1996-09-01

    The US Geological Survey (USGS) Energy Resource Surveys Program is currently conducting a five-year National Coal Resource Assessment project. Primary focus is on the quality and quantity of top-producing coal beds and coal zones in five of the nine major coal producing regions in the US. These regions include the (1) Northern and Central Appalachian Basin, (2) Gulf Coastal Plain, (3) Illinois Basin, (4) Colorado Plateau, and (5) Powder River Basin and Northern Great Plains.

  4. Interpretation of crustal structure from regional gravity anomalies, Ouachita Mountains area and adjacent Gulf coastal plain

    Energy Technology Data Exchange (ETDEWEB)

    Kruger, J.M.; Keller, G.R.

    1986-06-01

    A gravity data base from more than 35,000 stations was used to generate a series of regional gravity maps of the Ouachita Mountains area including adjacent parts of the craton and the Gulf coastal plain. These maps were used in conjunction with information from 96 wells, data from preexisting geophysical and geological investigations, and computer models to interpret four gravity profiles that transect the study area (approximately lat. 30-37/sup 0/N, long. 91.5-99/sup 0/W). These models, gravity maps, and previous investigations were then used to analyze various regional gravity anomalies and to interpret the gross crustal structure of the region and its tectonic implications. These data suggest that variably attenuated continental crust lies beneath the Gulf coastal plain, south of the Ouachita system gravity gradient, as opposed to typical continental crust of the craton north of this gradient. This variation in crustal structure probably reflects the complexity of Eocambrian and early Mesozoic rifting in the area. The Arkoma basin gravity minima may result from the combined effect of a late Paleozoic foreland basin and an Eocambrian northwest-trending, rift-related basin. The Ouachita system interior zone gravity maximum varies along strike of this orogenic belt. This anomaly appears to be a good indicator of the position of the Eocambrian continental margin and associated rift zone. Gravity anomalies in the Gulf coastal plain appear to be a combined effect of variable crustal attenuation, basins and uplifts, and mafic intrusions. Gravity maxima in the southern Oklahoma aulacogen result from uplifts and deep-seated mafic intrusions; gravity minima result from deep sedimentary basins.

  5. The crustal structure of the north-eastern Gulf of Aden continental margin: insights from wide-angle seismic data

    OpenAIRE

    Watremez, Louise; Leroy, Sylvie; Rouzo, Stephane; d'Acremont, E.; Unternehr, P.; Ebinger, C.; Lucazeau, F.; Al-lazki, A.

    2011-01-01

    P>The wide-angle seismic (WAS) and gravity data of the Encens survey allow us to determine the deep crustal structure of the north-eastern Gulf of Aden non-volcanic passive margin. The Gulf of Aden is a young oceanic basin that began to open at least 17.6 Ma ago. Its current geometry shows first- and second-order segmentation: our study focusses on the Ashawq-Salalah second-order segment, between Alula-Fartak and Socotra-Hadbeen fracture zones. Modelling of the WAS and gravity data (three pro...

  6. GuLF Study: The Gulf Long-Term Follow-Up Study

    Science.gov (United States)

    ... font size, or print this page. The GuLF STUDY Gulf Study Newsletter Learn more about the 33,000 people ... linkage to cancer and mortality records. The GuLF STUDY wants you! If you completed a telephone interview ...

  7. 76 FR 54375 - Safety Zone; Thunder on the Gulf, Gulf of Mexico, Orange Beach, AL

    Science.gov (United States)

    2011-09-01

    ... SECURITY Coast Guard 33 CFR Part 165 RIN 1625-AA00 Safety Zone; Thunder on the Gulf, Gulf of Mexico, Orange... establishing a temporary safety zone for a portion of the Gulf of Mexico for the waters off Orange Beach... Mexico, south of Orange Beach, Alabama to occur from October 6, 2011 through October 9, 2011. This...

  8. Vinna Basin

    Czech Academy of Sciences Publication Activity Database

    Honěk, J.; Franců, J.; Mikuláš, Radek; Pešek, J.; Sýkorová, Ivana; Tomanová-Petrová, P.

    Prague: Czech Geological Survey, 2014, s. 223-241 ISBN 978-80-7075-862-5 R&D Projects: GA ČR GA105/06/0653 Institutional support: RVO:67985891 ; RVO:67985831 Keywords : Tertiary basins * Czech Republic * Cenomanian and Tertiary lignite * geology * stratigraphy Subject RIV: DB - Geology ; Mineralogy

  9. A National Survey of Consumer Preferences for Branded Gulf Oysters and Risk Perceptions of Gulf Seafood

    OpenAIRE

    Petrolia, Daniel R.; Walton, William C.; Sarah, Acquah

    2014-01-01

    Three restaurant taste panels and an online consumer survey were conducted during 2012-2013 to assess whether Gulf consumers would be willing to pay a premium for place-name specific (i.e., “branded”) Gulf oysters over typical “generic” Gulf oysters, and whether consumers in other U.S. markets would be willing to pay for branded Gulf oysters compared to other U.S. branded oysters. Panelists in the two Gulf Coast taste panels had strong preferences for local oyster varieties when they were awa...

  10. Diseño e implementación de una estrategia didáctica para la enseñanza-aprendizaje de la Tabla Periódica y sus propiedades en el grado octavo utilizando las nuevas tecnologías TICs: estudio de caso en la Institución Educativa Alfonso López Pumarejo grupo 8-2

    OpenAIRE

    Causado Moreno, Ana Victoria

    2012-01-01

    Esta propuesta tiene como intención diseñar e implementar una estrategia didáctica para la enseñanza-aprendizaje de la Tabla Periódica y sus propiedades con el uso de las Tecnologías de la Información y de la Comunicación (TICs) en el grado octavo de la Institución educativa Alfonso López Pumarejo. La propuesta consiste en utilizar una herramienta virtual de aprendizaje como lo es la plataforma moodle, diseñar un curso virtual sobre el tema de tabla periódica para los estudiantes del grupo...

  11. Carbon sources and fates in the Gulf of Papua

    Science.gov (United States)

    Goni, M. A.; Monacci, N. M.; Gisewhite, R. A.; Ogston, A.; Crockett, J.; Nittrouer, C.

    2006-12-01

    Seabed sediments were collected along the particle-dispersal system associated with the Fly River-Gulf of Papua continental margin as part of the source to sink program in Papua New Guinea. Box and kasten cores were collected from the subaqueous delta located adjacent to the mouth of the Fly River as well as from the topset, foreset and bottomset regions of the active clinoform in the northern region of the Gulf of Papua. Analyses of elemental (organic carbon, inorganic carbon, nitrogen), stable isotopic (d13C and d15N), radiocarbon (14C), and biomarker (CuO oxidation products) signatures reveal significant differences in the content and composition of sedimentary organic matter (OM) along the dispersal system. The major sources of OM to the system appear to be remains of vascular plants, soil OM from the drainage basin, and materials derived from autochthonous productivity. The geographical contrasts in the concentrations and accumulation fluxes of these distinct types of allochthonous and autochthonous OM are presented in the context of patterns of sediment transport and deposition within the region. An overall OM budget for the whole dispersal system will be presented and its implication for carbon sequestration in fluvial-dominated continental margins discussed.

  12. Numerical Modeling of Methanogenesis at Walker Ridge, Gulf of Mexico

    Science.gov (United States)

    Glosser, D.; Cook, A.; Malinverno, A.; Daigle, H.

    2014-12-01

    Methane migration is a crucial link between locations of methane generation and natural gas hydrate reservoirs, yet migration mechanisms are poorly understood in the natural environment. In this study, we evaluate constraints on methanogenesis and methane diffusion through the development of a 1-dimensional diagenetic model of the Gulf of Mexico Gas Hydrate Joint Industry Project Site Walker Ridge 313 in the Gulf of Mexico. High saturation gas hydrate was confirmed at Walker Ridge from borehole logs, which measured both high compressional velocity and high resistivity in hydrate-bearing sand layers. Gas hydrate formation depends largely on organic matter concentration and methanogenesis rates. We will test how much organic matter is required to achieve gas hydrate saturations observed at Walker Ridge. Our model will incorporate methane generation around a sand layer as it is moves down through the sediment column. Variable porosity across the sediment column due to early diagenesis and sediment compaction will also be considered. Since methane solubility is higher in finer grained sediments due to smaller pore spaces, gas hydrate will form in the sand layer from methane transported by the relatively slow process of diffusion from finer grained layers. The results of this model are critical to the development of the basin scale simulation of overall methane flux based on the geometry of WR313. The simulation results will improve scientific characterization of how hydrates form and distribute within continental margin sediments.

  13. Integrated well-log, seismic, and biostratigraphic approach to sequence stratigraphy in Late Cenozoic expanded sections, Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Mitchum, R.M. Jr. (R M Mitchum Exploration Inc., Houston, TX (United States)); Sangree, J.B. (Sangree Exploration Inc., Houston, TX (United States)); Vail, P.R. (Rice Univ. Houston, TX (United States)); Wornar, W.W. (Microstrat Inc., Houston, TX (United States))

    1991-03-01

    Increased emphasis on well-log signatures and recognition criteria for stratigraphic sequence boundaries, systems tracts, and condensed sections in a sequence-stratigraphic context has enhanced facies interpretation and reservoir prediction capabilities. Integration of well logs with high-resolution biostratigraphy and paleobathymetry, high-quality seismic configuration data, and the latest eustatic cycle chart provides the best data base for sequence-stratigraphic analysis. This approach is particularly effective for thick, rapidly deposited slope and basin sediments, such as in the Plio-Pleistocene of the Gulf of Mexico basin. The general sequence-stratigraphic model consists of a depositional sequence with lowstand basin floor fan, slope fan, and prograding complex, transgressive systems tract, and highstand systems tract. Each systems tract is deposited at a predictable position in an interpreted eustatic cycle and has recognizable signatures in well logs and seismic data. Any given basin to which this model is applied is strongly controlled by its own tectonic subsidence and accommodation history, and by the type and rate of sediment supply, but the higher frequency eustatic cyclicity is superposed on the other basinal controls. A typical depositional model for the Plio-Pleistocene of the Gulf of Mexico basin is a diapir-controlled subbasin associated with a large contemporaneous expansion fault. The environment of deposition is closely related to the history of fault development. Reservoir sand distribution is characteristic and predictable for each systems tract. Carefully planned evaluation and completion techniques are based on these characteristics.

  14. Geohydrolic studies of Gulf Coast interior salt domes

    International Nuclear Information System (INIS)

    Disposal of high-level radioactive wastes in Gulf Coast salt domes requires that the cavities be free from groundwater dissolution for 250,000 years. Salinity variations of groundwater near selected domes were investigated. Saline groundwater anomalies (saline plumes) in aquifers pierced or uplifted by the dome may be the result of salt solution by groundwater. In the Northeast Texas salt dome basin electric logs of oil and gas wells have been used to estimate groundwater salinities in aquifers near selected domes. Thus far, the analyses have revealed saline groundwater anomalies around 4 of the 9 domes studied. Estimates of the rate of salt dissolution from domes associated with saline groundwater plumes indicate that less than 30 meters of salt will be removed from the upper surfaces of the dome in 250,000 years. Thus, these preliminary studies show that even apparently unstable domes may be sufficiently stable to serve as waste disposal sites. 6 figures

  15. Fishery potential of the Gulf of Kachchh

    Digital Repository Service at National Institute of Oceanography (India)

    Nair, V.R.; Govindan, K.; Ramaiah, Neelam; Gajbhiye, S.N.

    Fishery potential of the interior Gulf of Kachchh and adjacent creek regions was reported for the first time as baseline data for future ecological assessment. The experimental trawling and gill netting indicated that the inner Gulf (av. 7.8 kg...

  16. Water masses in the Gulf of Aden

    Digital Repository Service at National Institute of Oceanography (India)

    Al Saafani, M.A.; Shenoi, S.S.C.

    Hydrographic data collected from Gulf of Aden since 1920 have been compiled to identify and refine the definitions of water masses in the Gulf of Aden (GA) and to describe their spatio-temporal variability. Four water masses have been identified...

  17. Thermocline Regulated Seasonal Evolution of Surface Chlorophyll in the Gulf of Aden

    KAUST Repository

    Yao, Fengchao

    2015-03-19

    The Gulf of Aden, although subject to seasonally reversing monsoonal winds, has been previously reported as an oligotrophic basin during summer, with elevated chlorophyll concentrations only occurring during winter due to convective mixing. However, the Sea-Viewing Wide Field-of-View Sensor (SeaWiFS) ocean color data reveal that the Gulf of Aden also exhibits a prominent summer chlorophyll bloom and sustains elevated chlorophyll concentrations throughout the fall, and is a biophysical province distinct from the adjacent Arabian Sea. Climatological hydrographic data suggest that the thermocline, hence the nutricline, in the entire gulf is markedly shoaled by the southwest monsoon during summer and fall. Under this condition, cyclonic eddies in the gulf can effectively pump deep nutrients to the surface layer and lead to the chlorophyll bloom in late summer, and, after the transition to the northeast monsoon in fall, coastal upwelling driven by the northeasterly winds produces a pronounced increase in surface chlorophyll concentrations along the Somali coast. © 2015 Yao, Hoteit.

  18. Distribution of surficial sediments in the Southern Evoikos and Petalioi Gulfs, Greece

    Directory of Open Access Journals (Sweden)

    A.P. KARAGEORGIS

    2012-12-01

    Full Text Available A series of 123 surficial sediment samples from the Southern Evoikos and Petalioi Gulfs was studied for grain-size properties, carbonate content and mineralogical composition. Distribution of the sediments revealed two sedimentary provinces. The first concerns the Southern Evoikos Gulf, characterised by silty sediments with relatively low carbonate content. Quartz, feldspars, micas, clay and carbonate minerals are the major mineralogical components of the sediments. These sediments are the result of the Asopos River supply during Holocene and they contribute to the formation of smooth bottom morphology. The second province concerns the Petalioi Gulf (Northern and Southern, where the surficial sediments are mainly sandy and characterised by very high carbonate content. Their mineralogical composition reflects the lithology of the drainage basin. Since the modern terrigenous solid supply is limited, these sediments are not considered as products of recent sedimentation, but older deposits (relict sands. Their presence at such depths is justified by sea-level fluctuations and their preservation is due to the low sedimentation rate in the Petalioi Gulf, in combination with the strong hydrodynamic status of the area.

  19. Evolution of Pre-Jurassic basement beneath northern Gulf of Mexico coastal plain

    Energy Technology Data Exchange (ETDEWEB)

    Van Siclen, D.C.

    1990-09-01

    Data from the northern Gulf Coast region reveal a late Paleozoic wrench fault system along which North America (NA) moved southeast (present directions) alongside the northeastern edge of future South America (SA), to where collision with that continent converted a broad continental embankment off the Southern Oklahoma aulacogen into the Ouachita thrust belt. At the same time, Africa farther east, to which protruding SA was firmly joined, was continuing to advance the Appalachian thrusts on the opposite side of these faults. This relationship left no space between the American continents for the conventional remnant ocean or microcontinents. By Late Triassic time, however, extension south of the Ouachita Mountains was forming the series of Interior rift basins, at both ends of which new wrench faults transferred the extension southward to the DeSoto Canyon and South Texas rift basins. Genetically, the Ouachita thrusts are part of the subduction zone along the front of a former SA forearc basin, which continued to receive marine sediments into middle Permian. The Wiggins arch southeast of it is a sliver of that continent, left with NA when the Interior basin rifting jumped from that forearc basin southward across bordering outer basement highs to begin opening the deep Gulf of Mexico (GOM) basin. The Late Triassic crustal extension resulted from right-lateral translation of NA around the bulge of northwestern Africa. About 200 mi of this placed Cape Hatteras against Africa's Cap Blanc, in the configuration from which the magnetic data indicate spreading began in the Central North Atlantic Ocean. The reality of this translation is confirmed by widespread rifting at the same time in western North Africa and between all three northern Atlantic continents; this drew the tip of the Tethys sea southward to Cape Hatteras and led to deposition of voluminous Late Triassic red beds and evaporites along it.

  20. Alaska, Gulf spills share similarities

    International Nuclear Information System (INIS)

    The accidental Exxon Valdez oil spill in Alaska and the deliberate dumping of crude oil into the Persian Gulf as a tactic of war contain both glaring differences and surprising similarities. Public reaction and public response was much greater to the Exxon Valdez spill in pristine Prince William Sound than to the war-related tragedy in the Persian Gulf. More than 12,000 workers helped in the Alaskan cleanup; only 350 have been involved in Kuwait. But in both instances, environmental damages appear to be less than anticipated. Natures highly effective self-cleansing action is primarily responsible for minimizing the damages. One positive action growing out of the two incidents is increased international cooperation and participation in oil-spill clean-up efforts. In 1990, in the aftermath of the Exxon Valdez spill, 94 nations signed an international accord on cooperation in future spills. The spills can be historic environmental landmarks leading to creation of more sophisticated response systems worldwide

  1. Investigation of heavy metal pollutants at various depths in the Gulf of Izmit

    International Nuclear Information System (INIS)

    Highlights: • Monitoring seasonal variations in heavy metal pollution. • Heavy metal levels according to depth in seawater from the Gulf of Izmit. • Industrial activity and biological life co-exist in Izmit Bay. -- Abstract: In this study, we report results concerning the accumulation of heavy metals in seawater from Izmit Bay. The bay was divided into the three parts: the eastern, the central and the western basins. The goal of this study was to determine levels of heavy metals at various depths in the bay between April 2008 and May 2010. Liquid–liquid extractions were performed on seawater samples. An atomic absorption spectrophotometer was used to measure levels of six metals: lead, cadmium, chromium, iron, manganese and zinc. We applied our results to evaluate the status of pollution in the Gulf of Izmit. Significant seasonal differences in metal concentrations and higher concentrations of many metals in water near the shore are evidence for uncontrolled release of pollutants in the water

  2. Solar forcing of Gulf of California climate during the past 2000 yr suggested by diatoms and silicoflagellates

    Science.gov (United States)

    Barron, John A.; Bukry, David

    2007-01-01

    High-resolution records of the past 2000 yr are compared in a north–south transect (28° N to 24° N) of three cores from the eastern slopes of the Guaymas, Carmen, and Pescadero Basins of the Gulf of California (hereafter referred to as the “Gulf”). Evenly-spaced samples from the varved sediments in each core allow sample resolution ranging from ∼ 16 to ∼ 37 yr.

  3. Gulf of Mexico production still recovering

    International Nuclear Information System (INIS)

    This paper reports that the extent of damage caused by Hurricane Andrew to Gulf of Mexico oil and gas installations continues coming into focus. A preliminary tally by Minerals Management Service offers a reasonably complete summary of gulf production and pipeline systems damage detectable at the surface. MMS requires Outer Continental Shelf operators to inspect for underwater damage all platforms, pipelines, risers, and other structures within an 85 mile corridor along the path of Andrew's eye as it churned through the gulf. OCS operators have until Oct. 16 to submit plans for the Level II surveys

  4. Host rock geology and geochemistry of the Zona uranium occurrence, Peta Gulf Syncline (Upper Benue Trough), northeast Nigeria

    Science.gov (United States)

    Suh, C. E.; Dada, S. S.; Matheis, G.

    2000-11-01

    The Peta Gulf Syncline (Upper Benue Trough, northeast Nigeria) is a fault-bounded pull-apart sub-basin. The boundary faults are mainly northeast-southwest-trending en echelon strike-slip faults, truncated along their lengths by normal and tear faults with stepovers. The eastern marginal faults underwent rotation during sedimentation, whereas the steeply dipping western marginal faults were inactive. The Peta Gulf Sub-basin is filled by the Bima Sandstone Formation (Lower Cretaceous) which has three siliciclastic members: (i) B 1: medial fan coarse-grained to microconglomeratic sandstones; (ii) B 2: full fluvial medium-grained sandstones with minimal fines; and (iii) B 3: lacustrine and flood basin deposits comprising alternating fine-grained sandstones and siltstones/claystones. Sediment supply was from east to west and facies changes show a general fining in this direction. B 3 offers the most favourable environment/lithology for U concentration. The only significant U occurrence in the Peta Gulf Syncline is the Zona U anomaly, which occurs within transitional B 2-B 3 brecciated sandstones with wall rock alterations zones. The mineralised zone has elevated SiO 2, Fe, As, Ba and W levels but is depleted in the alkalis, Zr, Rb and Sr. This chemical zonation supports the epigenetic orgin of this anomaly.

  5. Alleghenian Reconstruction and Subsequent Evolution of the Gulf of Mexico, Bahamas, and Proto-Caribbean

    Science.gov (United States)

    Pindell, James L.

    1985-01-01

    A detailed model for the evolution of the Gulf of Mexico, the Bahamas and the Proto-Caribbean is built within the framework provided by a detailed initial Alleghenian (western Pangean) reconstruction and an accurate subsequent relative-motion history between North America and Gondwana (northern Africa and South America). The Alleghenian reconstruction closes all pre-Jurassic oceans; accounts for Jurassic attenuation of continental crust by restoring that attenuation to original prerift continental thicknesses; incorporates an improved Equatorial Atlantic fit between northern Brazil and the Guinea margin of Africa; quantitatively removes changes in shape of northern South America due to Late Cretaceous and Cenozoic accretion and internal deformation; includes pre-Mesozoic continental crust presently underlying the western Bahamas and southern Florida; and correlates Late Paleozoic geology of Yucatan with its neighboring continental masses. Extension occurred within the Gulf of Mexico from Late Triassic to earliest Cretaceous time, but seafloor spreading was delayed until the Late Callovian. This divided a single Gulf-wide salt basin into the Louann and Campeche salt provinces. The Yucatan block progressively rotated about 43 degrees counterclockwise away from the Texas-Louisiana margin around a pole in northern Florida. The Tamaulipas-Golden Lane-Chiapas fault zone of eastern Mexico is interpreted as the remains of an initially intracontinental transform system along which Yucatan migrated. Attenuated continental crust beneath southern Florida and the western Bahamas, termed here the Florida Straits block, migrated approximately 300 km out of the eastern Gulf, approximately along Central Atlantic flow lines. These rotations are consistent with recently suggested magnetic anomaly trends in the Gulf of Mexico (Shepherd et al., 1982; S. Hall, personal communication, 1984). The Proto-Caribbean formed synchronously by a fan-like rotation of Yucatan away from Venezuela.

  6. Seasonal Composite Chlorophyll Concentrations - Gulf of Maine

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This personal geodatabase contains raster images of chlorophyll concentrations in the Gulf of Maine. These raster images are seasonal composites, and were...

  7. Central Gulf of Alaska Rockfish Permit Program

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The North Pacific Fishery Management Council adopted the Central Gulf of Alaska Rockfish Program (Rockfish Program) on June 14, 2010, to replace the expiring Pilot...

  8. Northern Gulf Coast Digital Elevation Model

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — NOAA's National Geophysical Data Center (NGDC) is building high-resolution digital elevation models (DEMs) for select U.S. coastal regions in the Gulf of Mexico....

  9. Gulf of Mexico Ecosystem Status Report

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The Gulf of Mexico is one of the most ecologically and economically valuable marine ecosystems in the world and is affected by a variety of natural and...

  10. Anticlines in the US Gulf Coast [anticlineg

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset of anticlines is intended primarily for reference; it includes major structures such as those shown on Plate 2, Principal structural features, Gulf of...

  11. 2013 Gulf of Mexico SPCE angler survey

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This survey provides economic data related to marine recreational fishing in the Gulf of Mexico. The data collected include preference and opinion information...

  12. Saudis map $450 million gulf spill cleanup

    International Nuclear Information System (INIS)

    This paper reports on Saudi Arabia which has earmarked about $450 million to clean up Persian Gulf beaches polluted by history's worst oil spills, created during the Persian Gulf crisis. Details of the proposed cleanup measures were outlined by Saudi environmental officials at a seminar on the environment in Dubai, OPEC News Agency reported. The seminar was sponsored by the Gulf Area Oil Companies Mutual Aid Organization, an environmental cooperative agency set up by Persian Gulf governments. Meantime, a Saudi government report has outlined early efforts designed to contain the massive oil spills that hit the Saudi coast before oil could contaminate water intakes at the huge desalination plants serving Riyadh and cooling water facilities at Al Jubail

  13. ROE Gulf of Mexico Hypoxia Sample Locations

    Data.gov (United States)

    U.S. Environmental Protection Agency — This dataset describes dissolved oxygen levels in the Gulf of Mexico. Individual sampling sites are represented by point data. The background polygon shows areas...

  14. Southeast Gulf of Mexico Sperm Whale Study

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Large vessel surveys were conducted during the summers of 2012 and 2014 in the southeastern Gulf of Mexico north of the Dry Tortugas. Data were collected on the...

  15. Seismotectonics and Seismic Waves Transmision Characteristics of the Gulf of Mexico

    Science.gov (United States)

    Yamamoto, J.; Ruiz, V. H.

    2013-05-01

    Mexico's energy resources reside largely in the Gulf of Mexico Basin, one of the oil producing areas of greatest potential in the world. Recent scientific and technological advances on provide new insights that open new areas for exploration and exploitation that were unthinkable in the past, as in the case of the deepwater Gulf of Mexico. Investigate the characteristics of this region from different perspectives should be a national priority. This research is an effort in that direction. This work consists of two parts in the first we examine the spatial distribution of seismicity and focal mechanisms of major earthquakes in the Gulf of Mexico (GM). In particular we discuss the mechanism of rupture of the event (Mw 5.9) of 10 September 2006 located off the coast of Florida, United States of America and the May 23, 2007 (Mw 5.4) off the coast of Tuxpan, Veracruz. These two are the most relevant events occurred within the basin of GM in recent years. In the second part we study the inelastic attenuation of seismic signals in the GM by analyzing the decay of the coda of the S wave and surface waves in some cases. The attenuation is estimated by calculating the quality factor Q for different paths within the basin in the frequencies range of 0.3 to 4.0 Hz. It is assumed that the Q factor is governed by the equation Q(f)=Qof**n where Qo is the value of Q (f) at 1 Hz. The calculation uses the broadband digital records of five events of medium magnitude (5.2 <= Mw <= 7) occurred off the coast of Florida and Veracruz recorded by the IRIS and SSN networks. Data from the 2010 Haiti earthquake is used for comparison purposes.

  16. Hydrodynamic Modeling of the Gulf of Aqaba

    OpenAIRE

    Hesham El-Badry; Ahmed Sayed Mohamed Ahmed; Mohamed E. Abou-Elhaggag

    2012-01-01

    The Gulf of Aqaba (GOA) is unique as it contains significant percentage of the world’s natural marine biodiversity. This unique environment is potentially vulnerable to pollution particularly at its northern tip. One of the major activities affecting the environment of the gulf is the man-made desalination plants that abstract sea water and dispose desalinated brine. In this context, the paper discusses the impact of the abstract and disposal activities on the GOA environment. A 3D hydrodynam...

  17. Chemosymbiotic species from the Gulf of Cadiz

    OpenAIRE

    Rodrigues, C. F.; A. Hilário; M. R. Cunha

    2013-01-01

    Previous work in the mud volcanoes from the Gulf of Cadiz (South Iberian Margin) revealed a high number of chemosymbiotic species, namely bivalves and siboglinid polychaetes. In this study we give an overview of the distribution and life styles of these species in the Gulf of Cadiz, determine the role of autotrophic symbionts in the nutrition of selected species using stable isotope analyses (δ13C, δ15N and δ34S) and investigate the intra-specific variation of isotope signat...

  18. Climate forcing, primary production and the distribution of Holocene biogenic sediments in the Gulf of California

    Science.gov (United States)

    Douglas, Robert; Gonzalez-Yajimovich, Oscar; Ledesma-Vazquez, Jorge; Staines-Urias, Francisca

    2007-01-01

    The Gulf of California is a marginal seaway under the influence of a monsoon climate that produces cool, dry winters and warm, humid summers. Winds, tidal mixing and coastal-trapped waves forced by climate and the Pacific Ocean control nutrient advection and primary productivity (PP). Strong northwest winds from the subtropical East Pacific High Pressure system begin in November and last until April and drive coastal upwelling along the mainland margin, especially in the central and southern Gulf. In the northern Gulf, particularly around the midrift island, tidal mixing and turbulence occurs year round, advecting nutrients into the mixed layer and high productivity. During summer and early fall months, winds are variable, of less intensity and mainly blow cross-basin except in the most northern Gulf. Summer PP is generally low in the central and southern Gulf except along the mainland where coastal-trapped waves associated with tropical surges and hurricanes generate mixing over the continental shelf. Mesoscale eddies or gyres often associated with jets and filaments extend to depths of 1000 m and transport nutrient-enriched upwelled waters and plankton detritus across the Gulf. The largest and most persistent gyres rotate in an anti-cyclonic direction (east to west) and are a principal source of the plankton export to the peninsula margin. Two major biogenic sediment patterns are present in core-top sediments. Hemipelagic biosiliceous-rich muds are accumulating beneath upwelling areas of high productivity in the central Gulf and along the mainland margin. Calcium carbonate- and organic carbon-rich (OC) sediments are concentrated along the peninsula margin, generally beneath lower productivity waters with the highest OC content in areas with the lowest productivity. The high, uniform biosiliceous content in Guaymas basin, extending southward into Carmen basin reflects the redistribution by mesoscale gyres of phytoplankon debris produced in mainland coastal

  19. Major reproductive health characteristics in male Gulf War Veterans. The Danish Gulf War Study

    DEFF Research Database (Denmark)

    Ishøy, T; Andersson, A M; Suadicani, Poul Vilhelm;

    2001-01-01

    The male reproductive system could have been affected by various hazardous agents and exposures during and in the aftermath of the Persian Gulf War scenario. We tested the hypothesis that, compared to controls, male Danish Gulf War Veterans would have adverse sex hormone levels, decreased fertility...

  20. Seismic stratigraphy and salt tectonics of upper Continental Slope, East Breaks flexure trend, Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Gardiner, W.B.

    1986-05-01

    A study of more than 1200 of 72-fold, migrated, seismic reflection profiles, from the eastern part of the East Breaks flexure trend, Gulf of Mexico, indicates that, although individual seismic reflectors cannot be traced across the entire area, seismic depositional units can be recognized and correlated from basin to basin in most instances. Three tentative conclusions are evident from this study: (1) salt diapirs appear to have grown through a series of intermittent movements to form structurally separate intraslope basins; (2) sedimentation is probably channeled by differential dome growth, which creates local stratigraphic differences between basins; and (3) packages of distinctive seismic depositional units can be successfully used to map sediment cycles between separate basins. Fluctuations of Pleistocene sea level appears to be the dominate depositional control on the upper continental slope in this area. During high sea level stands, turbidity currents were confined to depressions between diapirs, whereas pelagic deposition blanketed the slope. But during low sea level stands, sediment bypassed the shelf and deposited directly onto the upper slope, which increased the sediment load and helped initiate diapirism. Repeated sea level fluctuation would then lead to the cyclic pattern of seismic depositional packages that is commonly seen on upper slope seismic records.

  1. Modeling Circulation Patterns that Influence Connectivity of Remote Ecosystems in the Wider Caribbean Region and the Gulf of Mexico

    Science.gov (United States)

    Kourafalou, V. H.; Halliwell, G.; Hogan, P.; Kang, H.; Schiller, R.; Paris, C.

    2008-05-01

    The Wider Caribbean Region (WCR) comprises the insular and coastal States and Territories with coasts on the Caribbean Sea and Gulf of Mexico as well as waters of the Atlantic Ocean adjacent to these States and Territories and includes 28 island and continental countries. The main sub-basins are inter-connected with a large scale current system that includes the North Brazil Current, the Caribbean Current, the Loop Current and the Florida Current. This current system and associated rings and eddies provide the physical background for the connectivity of WCR ecosystems that can be at great distances from each other. A hierarchy of regional numerical models based on the HYbrid Coordinate Ocean Model (HYCOM) has been developed to study the physical transport mechanisms and support efforts under the Integrated Ocean Observing System (IOOS): CARIB-HYCOM (WCR region); GoM-HYCOM (Gulf of Mexico region), Northern Gulf of Mexico (NGoM region), WFS-HYCOM (West Florida Shelf region), SoFLA-HYCOM (South Florida region) and FKEYS- HYCOM (Florida Keys region). The models range in resolution from 900m to 4 km and they are gradually nested to Atlantic basin-wide and global HYCOM models of 7-8 km resolution. This multi-nested approach allows the detailed study of regional processes, while maintaining the interaction with surrounding regions. This is an important methodology in the Wider Caribbean Region, where the presence of complicated topography and the large scale current system dictate strong coastal to offshore interactions and inter-basin exchanges. The multi-nested modeling approach has allowed the study of circulation and transport processes in the Caribbean Sea and the Gulf of Mexico. Examples will concentrate on the transport of low salinity, nutrient rich waters originating at the Amazon and Mississippi Rivers and the connectivity pathways that influence larval transport. Boundary condition and data assimilation needs for pre-operational forecasting of such pathways

  2. Contamination from gold and platinum-group metals mining in the Gulf of Darién, Colombia

    Science.gov (United States)

    Vasquez-Bedoya, L.; Palacio Baena, J.

    2013-12-01

    Gulf of Darién, triangular southernmost extension of the Caribbean Sea, bounded by Panama on the southwest and by Colombia on the southeast and east. The Gulf is made up of 17 municipalities in the department of Choco and Antioquia. The Gulf of Darién is a geostrategic region, rich in biodiversity, known for its natural resources of minerals, oil, lumber as well as its water and fertile land. The Darién also acts as the bridge between South America and Central America and has access to the Pacific Ocean and the Caribbean Sea. The economy in the region is based mainly on agribusinesses, tourism and mining activities, mainly the 'mining of gold and platinum-group metals'. In our study we determined the degree of trace element contamination in estuarine sediment samples originated from mining activities and municipal waste water discharges of effluents on the gulf of Darién. . Surface samples were taken from 17 locations through the entire Gulf. Grain size, Corg, Ag, Al, Ca , Cr, Cu, Fe, Mg, Mn, Na, Ni, Pb and Zn concentrations were analyzed, and enrichment factors (EF) as well as geo-accumulation indices (Igeo) were calculated. Concentrations of Pb, Zn, Ni, Cu and Cr show levels that are consistent with those typically found in urbanized marine environments. EF and Igeo values revealed that the Gulf is extremely contaminated with Ag and moderately contaminated with Cr and Zn. The sources of Cr, Ag, Hg and Zn are associated with the development of mining activities in the Atrato River basin. The observed enrichment of Ag may be explained as a residue of the extraction of gold and platinum-group metals.

  3. Gulf Coast hurricane activity and climate variability during the last half of the Holocene

    Science.gov (United States)

    Lane, P.; Donnelly, J. P.

    2011-12-01

    The dominant timescales of variability in a 4500-year sediment-based storm chronology from the northeastern Gulf of Mexico are identified, and relationships between storm frequency and climate are explored. Changes in the frequency of large storm surge deposits in the record likely represent variability in the intensity distribution of hurricanes impacting the site during the late Holocene. Significant variability at approximately 200 and 1000-year timescales that was detected in the storm record is shared by numerous Holocene climate records including reconstructions of Loop Current penetration into the Gulf of Mexico. Intense storm landfalls were most frequent around 3.7 ka, between 2.7 and 2.4 ka, and around 0.7 ka when foraminiferal proxies of mixed layer depth indicate a more permanent residence of the Loop Current within the northeastern Gulf. Migrations of the Loop Current would exercise control over regional hurricane activity by changing the thermal structure of the upper ocean and influencing the role of storm-induced upwelling on hurricane intensification. Other factors that influenced regional and Atlantic basin-wide hurricane activity include the El Niño/Southern Oscillation and the position of the Inter-Tropical Convergence Zone. Many authors have suggested that bicentennial and millennial-scale climate variability may have been driven ultimately by changes in solar irradiance. Thus, low-frequency variability in Atlantic hurricane activity may be an expression of the climate system's response to exogenous forcing.

  4. The United States and the Arab Gulf Monarchies

    International Nuclear Information System (INIS)

    The United States has enduring strategic interests in the Persian Gulf region. To understand these interests and the Usa policy towards the Arab Gulf Monarchies, the french institute of international relations (IFRI) proposes this document. The following chapters are detailed: the United States and the Arab Gulf Monarchies, overview, Chief Unites States Objective: Access to oil, re-evaluating United States Foreign Policy in the Gulf, the second term (Usa strategy). (A.L.B.)

  5. Reproductive health and pregnancy outcomes among French gulf war veterans

    OpenAIRE

    Bégassat Marion; De Vigan Catherine; Jutand Mathe-Aline; Verret Catherine; Bensefa-Colas Lynda; Brochard Patrick; Salamon Roger

    2008-01-01

    Abstract Background Since 1993, many studies on the health of Persian Gulf War veterans (PGWVs) have been undertaken. Some authors have concluded that an association exists between Gulf War service and reported infertility or miscarriage, but that effects on PGWV's children were limited. The present study's objective was to describe the reproductive outcome and health of offspring of French Gulf War veterans. Methods The French Study on the Persian Gulf War (PGW) and its Health Consequences i...

  6. Diseño y aplicación de ambiente virtual de aprendizaje en el proceso de enseñanza - aprendizaje de la física en el grado décimo de la I.E. Alfonso López Pumarejo de la ciudad de Palmira

    OpenAIRE

    Rico González, Carlos Arturo

    2011-01-01

    La enseñanza de la asignatura de física en la Institución Educativa Alfonso López Pumarejo (IEALP) se ha caracterizado por el uso del tablero y marcador como únicos recursos didácticos, esta situación ha contribuido a la desmotivación y desinterés por parte de los estudiantes frente a su proceso de aprendizaje. El presente proyecto generó una serie de herramientas didácticas basadas en la incorporación de las Tecnologías de la Información y la Comunicación (TIC) a través de la creación de un ...

  7. Evidence for deep-water evaporite deposition in the Miocene Kareem Formation, Gemsa basin, eastern Egypt

    Energy Technology Data Exchange (ETDEWEB)

    May, J.A.; Stonecipher, S.A.; Steinmetz, J.C. (Marathon Oil Co., Littleton, CO (United States)); Dyess, J.N. (Marathon Petroleum Egypt, Maadi (Egypt))

    1991-03-01

    The correct interpretation of intercalated Miocene siliciclastics and evaporites of Gemsa basin is crucial for understanding early rift tectonics of the Gulf of Suez, pinpointing the timing of isolation of the Gulf from the Mediterranean, and developing exploration plays. Evaporites of the Kareem Formation comprise celestites and massive, 'chicken-wire,' and laminated anhydrites. Although previously interpreted as sabkha deposits; sedimentologic, petrographic, and paleontologic analyses indicate these evaporites more likely formed in a submarine setting. Marls that encase the evaporites contain a diverse and abundant assemblage of nannoplankton, planktonic foraminifera, diatoms, pteropods, and fish scales indicative of basinal deposition. Associated turbidites also denote deep-water sedimentation. The paucity of benthic diatoms and foraminifera, plus the presence of unburrowed shales, phosphate nodules, early ferroan carbonate cements, and authigenic pyrite, suggest periodic anoxic, or at least disaerobic, bottom waters. These sequences probably represent partial isolation of the Gulf of Suez by middle Miocene, producing periodic basin restriction and evaporative drawdown. Episodes of increasing salinity likely caused the progressive decreases in foram abundance and diversity in marls beneath the anhydrites, culminating in subaqueous evaporite formation. Diverse, indigenous nannoplankton assemblages from shale seams within the anhydrites suggest Gemsa basin was stratified; shallow open-marine conditions coexisted with anhydrite crystallization from deeper hypersaline waters.

  8. Coastal vulnerability assessment of the Northern Gulf of Mexico to sea-level rise and coastal change

    Science.gov (United States)

    Pendleton, E.A.; Barras, J.A.; Williams, S.J.; Twichell, D.C.

    2010-01-01

    A coastal vulnerability index (CVI) was used to map the relative vulnerability of the coast to future sea-level rise along the Northern Gulf of Mexico from Galveston, TX, to Panama City, FL. The CVI ranks the following in terms of their physical contribution to sea-level rise-related coastal change: geomorphology, regional coastal slope, rate of relative sea-level rise, historical shoreline change rate, mean tidal range, and mean significant wave height. The rankings for each variable are combined and an index value is calculated for 1-kilometer grid cells along the coast. The CVI highlights those regions where the physical effects of sea-level rise might be the greatest. The CVI assessment presented here builds on an earlier assessment conducted for the Gulf of Mexico. Recent higher resolution shoreline change, land loss, elevation, and subsidence data provide the foundation for a better assessment for the Northern Gulf of Mexico. The areas along the Northern Gulf of Mexico that are likely to be most vulnerable to sea-level rise are parts of the Louisiana Chenier Plain, Teche-Vermillion Basin, and the Mississippi barrier islands, as well as most of the Terrebonne and Barataria Bay region and the Chandeleur Islands. These very high vulnerability areas have the highest rates of relative sea-level rise and the highest rates of shoreline change or land area loss. The information provided by coastal vulnerability assessments can be used in long-term coastal management and policy decision making.

  9. Seismic images of the base of the gas hydrate stability zone in Northwest walker ridge, Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    McConnell, D.R. [Fugro GeoServices, Inc (United States); Kendall, B.A. [Oil and Gas Development Corp., Kerr-McGee, Islamabad (Pakistan)

    2002-10-01

    The gas hydrate stability zone, the zone below the sea-floor where gas and water should form gas hydrate is predicted to be present in shallow sediments in deep-water areas around the world, including the deep-water Gulf of Mexico. Few, if any, bottom simulating reflectors (BSR) or other manifestations of the gas hydrate stability zone have been interpreted in the Gulf of Mexico. We show convincing images of the base of the gas hydrate stability zone extracted from exploration 3-D data in Northwest Walker Ridge in the Gulf of Mexico. This area is on the margin of an uplifted and compressed mini-basin and in the vicinity of numerous giant gas mounds at the sea-floor. Shallow stratigraphy includes laterally extensive, steeply dipping basin floor silts and silty sands. This paper shows images of hydrate-trapped gas at multiple reflectors at depths that are coincident with the predicted base of the hydrate stability zone if modeled with a geothermal gradient of 19.6{+-}0.5 deg C/km. A BSR is seen in the seismic data in vertical section, but the more convincing images of the base of gas hydrate stability are seen in map view. (authors)

  10. Gulf Canada Resources Limited 1998 annual report

    International Nuclear Information System (INIS)

    A review of operations in 1998 and financial information from Gulf Canada Resources Limited is provided to keep shareholders abreast of company performance. Gulf Canada Resources Limited explores for, develops, produces and markets conventional and synthetic crude oil, natural gas and natural gas liquids. In 1998, the company's main operating centres were in western Canada (where it owns a nine per cent interest in the Syncrude Joint Venture), Indonesia, the North Sea and Australia. The report summarizes the company's energy resource activities, presents a detailed review of operations, and provides consolidated financial statements, and common share information. Although Gulf Canada Resources sold $ 1.2 billion worth of non-producing assets during the year, year end proved reserves of 838 million barrels of oil equivalent were less than ten per cent lower than a year earlier, reflecting reserve additions of 100 million barrels of oil equivalent. tabs., figs

  11. Deep Eddies in the Gulf of Mexico

    Science.gov (United States)

    Furey, H. H.; Bower, A. S.; Perez-Brunius, P.; Hamilton, P.

    2014-12-01

    A major Lagrangian program is currently underway to map the deep (1500-2500 m) circulation of the entire Gulf of Mexico. Beginning in 2011, more than 120 acoustically tracked RAFOS floats have been released in the eastern, central and western Gulf, many in pairs and triplets. Most floats are programmed to drift for two years, obtaining position fixes and temperature/pressure measurements three times daily. More than 80 floats have completed their missions, and results from the trajectories will be described with a focus on mesoscale eddying behavior. In particular, the first-ever observations of deep energetic anticyclonic eddies (possibly lenses) forming at and separating from a northeastward-flowing boundary current west of Campeche Bank will be discussed. The existence of these eddies has major implications for exchange between the continental slope and interior Gulf. The project is being supported by the U.S. Bureau of Ocean Energy Management (BOEM).

  12. 76 FR 30705 - Gulf of Mexico Citizen Advisory Committee; Request for Nominations to the Gulf of Mexico Citizen...

    Science.gov (United States)

    2011-05-26

    ... AGENCY Gulf of Mexico Citizen Advisory Committee; Request for Nominations to the Gulf of Mexico Citizen... considered for appointment to the Gulf of Mexico Citizen Advisory Committee (GMCAC). Vacancies are... Mexico Citizen Advisory Committee (GMCAC) to provide independent citizen advice to the EPA...

  13. Wetlands of the Gulf Coast

    Science.gov (United States)

    2001-01-01

    This set of images from the Multi-angle Imaging SpectroRadiometer highlights coastal areas of four states along the Gulf of Mexico: Louisiana, Mississippi, Alabama and part of the Florida panhandle. The images were acquired on October 15, 2001 (Terra orbit 9718)and represent an area of 345 kilometers x 315 kilometers.The two smaller images on the right are (top) a natural color view comprised of red, green, and blue band data from MISR's nadir(vertical-viewing) camera, and (bottom) a false-color view comprised of near-infrared, red, and blue band data from the same camera. The predominantly red color of the false-color image is due to the presence of vegetation, which is bright at near-infrared wavelengths. Cities appear as grey patches, with New Orleans visible at the southern edge of Lake Pontchartrain, along the left-hand side of the images. The Lake Pontchartrain Bridge runs approximately north-south across the middle of the lake. The distinctive shape of the Mississippi River Delta can be seen to the southeast of New Orleans. Other coastal cities are visible east of the Mississippi, including Biloxi, Mobile and Pensacola.The large image is similar to the true-color nadir view, except that red band data from the 60-degree backward-looking camera has been substituted into the red channel; the blue and green data from the nadir camera have been preserved. In this visualization, green hues appear somewhat subdued, and a number of areas with a reddish color are present, particularly near the mouths of the Mississippi, Pascagoula, Mobile-Tensaw, and Escambia Rivers. Here, the red color is highlighting differences in surface texture. This combination of angular and spectral information differentiates areas with aquatic vegetation associated with poorly drained bottom lands, marshes, and/or estuaries from the surrounding surface vegetation. These wetland regions are not as well differentiated in the conventional nadir views.Variations in ocean color are apparent in

  14. Generation of Wind Waves in the Persian Gulf: A Numerical Investigation

    Science.gov (United States)

    Liao, Y.; Kaihatu, J. M.

    2010-12-01

    The Persian Gulf is a long shallow basin located between the Arabian Peninsula and Iran. Wind-wave generation processes in the region are often affected by the shamal, a strong wind caused by the passage of cold fronts over the mountains of Turkey and Kurdistan. This can set up sudden energetic wind seas, hampering marine traffic. It is not immediately clear whether present wind-wave models can predict this intense, short-term growth and evolution under these conditions. Furthermore, few wave measurements or models studies have been performed in this area. In advance of a wind-wave generation experiment to be conducted off the Qatar coast, we performed a climatological study of the wind wave environment in the Persian Gulf. Using the SWAN wave model as a baseline of the state of the art, five years (2004-2008)of wind field model hindcasts from COAMPS are used as forcing.To investigate the sensitivity of the results to bathymetry, the climatological analysis was run twice more, with refraction or wave breaking deactivated, in turn. The results do not show significant differences with and without refraction, which implies the wind-wave process in Persian Gulf is less dominated by the variation of bathymetry. However the results show that a large amount of wave is dissipated by wave breaking. Wide, flat and shallow bathymetry in Persian Gulf results in a long-fetch scenario, particularly for waves arriving from the northwest. It implies that long period wind-generated waves can be fully generated in this region. Wave height is therefore fully grown by the long-fetch condition, so as to lead in higher possibility of wave breaking and energy dissipation.

  15. A High Resolution Geophysical Study of the Offshore Western Gulf of Corinth Rift

    Science.gov (United States)

    McNeill, L.; Cotterill, C.; Stefatos, A.; Henstock, T.; Bull, J.; Collier, R.; Papatheodorou, G.; Georgiopoulou, A.; Ferentinos, G.

    2003-12-01

    The western Gulf of Corinth has generated recent debate in terms of distribution of extensional strain, interactions between active faults and fault geometry. Onshore data suggest that faults do not accommodate extensional strain of the magnitude suggested by geodetic measurements. Recently acquired high resolution geophysical data in the western Gulf of Corinth, including Reson Seabat 8160 50 kHz multibeam bathymetry (with sidescan collected simultaneously) and sparker and boomer seismic profiles, will allow a detailed study of faulting relationships, fault propagation history and associated sedimentological processes. Multibeam data indicate the complex axial and tributary channel pattern of the gulf as well as revealing the surface expression of active faults on both margins and within the basin centre. Several fault tips are evident, including the Aigion fault which has been surveyed in great detail with boomer lines spaced between 25-100 m. The fault tip is complex with multiple synthetic and antithetic splays. The post-lowstand transgressive surface is clearly imaged and therefore fault growth rates can be established. Gas-related features are common, including pockmarks and mud volcanoes. To the east, displacement on the eastern tip of the Eliki fault decreases rapidly offshore and a splay of the Derveni fault is observed. A major S-dipping antithetic fault opposite the Eastern Eliki fault has clear bathymetric expression and is locally associated with a prominent basement ridge. This fault may make a significant contribution to extensional strain in this part of the rift. In the centre of the basin, sediments are deformed by multiple minor faults with seafloor displacement. Ultimately, high resolution offshore interpretations can be integrated with regional datasets and existing data (e.g., geomorphic, paleoseismological and sedimentological) onshore and used to better assess rift deformation models, rift evolution and local seismic hazards.

  16. Gulf International Conference on Applied Mathematics 2013

    CERN Document Server

    Advances in Applied Mathematics

    2014-01-01

    This volume contains contributions from the Gulf International Conference in Applied Mathematics, held at the Gulf University for Science & Technology. The proceedings reflects the three major themes of the conference. The first of these was mathematical biology, including a keynote address by Professor Philip Maini. The second theme was computational science/numerical analysis, including a keynote address by Professor Grigorii Shishkin. The conference also addressed more general applications topics, with papers in business applications, fluid mechanics, optimization, scheduling problems, and engineering applications, as well as a keynote by Professor Ali Nayfeh.

  17. Gulf Coast Clean Energy Application Center

    Energy Technology Data Exchange (ETDEWEB)

    Dillingham, Gavin

    2013-09-30

    The Gulf Coast Clean Energy Application Center was initiated to significantly improve market and regulatory conditions for the implementation of combined heat and power technologies. The GC CEAC was responsible for the development of CHP in Texas, Louisiana and Oklahoma. Through this program we employed a variety of outreach and education techniques, developed and deployed assessment tools and conducted market assessments. These efforts resulted in the growth of the combined heat and power market in the Gulf Coast region with a realization of more efficient energy generation, reduced emissions and a more resilient infrastructure. Specific t research, we did not formally investigate any techniques with any formal research design or methodology.

  18. Star Formation in the Gulf of Mexico

    CERN Document Server

    Armond, Tina; Bally, John; Aspin, Colin

    2011-01-01

    We present an optical/infrared study of the dense molecular cloud, L935, dubbed "The Gulf of Mexico", which separates the North America and the Pelican nebulae, and we demonstrate that this area is a very active star forming region. A wide-field imaging study with interference filters has revealed 35 new Herbig-Haro objects in the Gulf of Mexico. A grism survey has identified 41 Halpha emission-line stars, 30 of them new. A small cluster of partly embedded pre-main sequence stars is located around the known LkHalpha 185-189 group of stars, which includes the recently erupting FUor HBC 722.

  19. Gulf Islands Wilderness study area : Gulf Island National Wildlife Refuges : Wilderness study report

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This document is a brief report on a wilderness study area located in the Gulf Island National Wildlife Refuges. It discusses the history of the study area, its...

  20. Intrinsic low-frequency variability of the Gulf Stream

    Directory of Open Access Journals (Sweden)

    G. Quattrocchi

    2012-03-01

    Full Text Available In this paper a process study aimed at analyzing the low-frequency variability of intrinsically oceanic origin of the Gulf Stream (GS and GS extension (GSE is presented. An eddy-permitting reduced-gravity nonlinear shallow water model is implemented in an idealized North Atlantic Ocean, with schematic boundaries including the essential geometric features of the coastline and a realistic zonal basin width at all latitudes. The forcing is provided by a time-independent climatological surface wind stress obtained from 41 years of monthly ECMWF fields. The model response yields strong intrinsic low-frequency fluctuations on the interannual to decadal time scales. The modelled time-averaged GS/GSE flows are found to exhibit several features that can also be deduced from satellite altimeter data, such as the Florida Current seaward deflection, the GS separation at Cape Hatteras, and the overall structure of the GSE. The intrinsic low-frequency variability yields two preferred states of the GSE differing in latitudinal location that also have their counterpart in the altimeter data. A preliminary analysis of the variability in terms of dynamical systems theory is carried out by using the lateral eddy viscosity as the control parameter. A complex transition sequence from a steady state to irregular low-frequency variability emerges, in which Hopf and global bifurcations can be identified.

  1. EXPORTACIÓN DE SEDIMENTOS DESDE CUENCAS HIDROGRÁFICAS DE LA VERTIENTE ORIENTAL DEL GOLFO DE URABÁ: INFLUENCIAS CLIMÁTICAS Y ANTRÓPICAS SEDIMENT EXPORTS FROM THE EASTERN BASIN IN THE GULF OF URABA: CLIMATIC AND ANTHROPOGENIC INFLUENCES

    Directory of Open Access Journals (Sweden)

    Andrea Arroyave-Rincón

    2012-06-01

    Full Text Available En este artículo se analizaron series de tiempo mensuales de precipitación (mm, caudal (m³/s y exportación de sedimentos (kton/día en cuencas de la vertiente oriental del golfo de Urabá. Se analizó la dinámica de la exportación de sedimentos, la relación caudal-exportación y caudal-precipitación. Se infirió el papel de fenómenos atmosféricos estacionales y multianuales (El Niño-Oscilación Sureña, ENOS, y factores antrópicos. Se encontraron variabilidades intra-anuales significativas (ANOVA: pThis article reports on a time-series analysis of monthly precipitation (mm, river discharge (m³/s and sediment export (kton/day in Urabá Gulf. We analyzed the dynamics of sediment exports relative to river discharge, and the dynamics of this latter variable relative to precipitation. We inferred the role of seasonal and multi-annual atmospheric drivers, and anthropogenic factors. We found significant intra-annual variability (ANOVA: p<0.001 consistent with the movement of the Inter-Tropical Convergence Zone. The Pearson correlation between variables showed direct and significant relationships (p<0.001. The ENSO did not influence precipitation. Using aerial-photographs, we analyzed anthropogenic factors in the municipalities of Apartadó (1961-2005 and Chigorodó (1961-2007, finding up to a 90% forest-cover loss. Using double-mass graphs, it was observed an increase in slope steepness (during mid 90’s, consistent with an increase in sediment export rate relative to discharge, thus suggesting that there was a significant effect of human factors, such as deforestation.

  2. Reconstruction of the Gulf of Lions margin during the Messinian Salinity Crisis

    Science.gov (United States)

    Steckler, M. S.; Lofi, J.; Mountain, G. S.; Ryan, W. B. F.; Berné, S.; Gorini, C.

    2003-04-01

    The desiccation of the Mediterranean Sea during the Messinian Salinity Crisis from 5.9 to 5.3 Ma subaerially exposed its continental margins. In regions near major rivers, the margins were eroded into dissected subaerial ramps. Farther seaward, the deep Mediterranean basin received extensive evaporitic deposits along with clastic debris shed from the margins. The fluvial landscape at the former continental margins and the deep evaporite basins were then rapidly resubmerged at by the flooding of the Mediterranean at the end of the crisis. Since that time, rivers have fed a continuous supply of sediment, rebuilt the margins and buried the erosion surface and Messinian sediments. The geometry of the Messinian erosion surfaces and strata has been progressively deformed by subsidence, compaction, sediment loading and tectonics. Seismic reflection profiles show a large sag in the Messinian erosion surface beneath the Gulf of Lions margin that was clearly not present at 5.3 Ma. This geometry highlights the need to reconstruct the past bathymetry and stratigraphy. In order to address this problem, we have performed preliminary 2D backstripping of several profiles constructed from a TotalFinaElf MCS survey on the shelf and the CALMAR project survey farther offshore. Our reconstructions provide estimates of the geometry of the margin during the Salinity Crisis and support a two-stage model for the desiccation of the Western Mediterranean. During the first stage the Western Mediterranean was drawn down to the depth of a sill separating the Eastern and Western basins; during the second phase the Western basin was fully desiccated and the upper salt was deposited. Our reconstructions indicate the presence of two erosion surfaces that correspond to these two phases. We have used river thalwegs in the reconstructed profiles to define the incised lower erosion surface as a concave up surface that averages ˜0.6^o dip and ends at the evaporites at a depth of 1800--1900 m. The first

  3. Using Multi-Species Foraminiferal δ18O to Reconstruct Hydrologic Changes in the Gulf of Panama From LGM to Present

    Science.gov (United States)

    Benway, H. M.; Mix, A. C.

    2002-12-01

    Currently, an excess in precipitation minus evaporation (P-E) maintains a low-salinity surface layer and a shallow pycnocline in the Gulf of Panama. In contrast, the Caribbean has high salinity due to high evaporation relative to precipitation. The strong salinity gradient between these two regions is sustained by northeasterly trade winds, which carry evaporated moisture from the Caribbean over the Panama Isthmus and into the Gulf of Panama, where high SSTs attract the moisture-laden air masses. This leads to atmospheric convection and heavy rainfall on the Pacific side of the Isthmus in the Gulf of Panama. Since the majority of the rainfall in this region originates as water vapor in the Caribbean, changes in vapor transport can be estimated by changes in upper ocean structure in the Gulf of Panama. A multi-species approach is used in a Panama Basin sediment core to reconstruct changes in cross-isthmus vapor transport from LGM to present. We measure δ18O in two species of planktonic foraminifera, one that lives at the surface and one that lives at the base of the pycnocline, in order to estimate the isotopic contrast across the pycnocline, which is directly related to net precipitation in the Gulf of Panama (i.e., an increase in δ18O contrast between the sea surface and the base of the pycnocline is associated with an increase in P-E).

  4. Eutrophication: State of the Gulf of Maine

    Science.gov (United States)

    Cultural eutrophication is an ecosystem response to increases in nutrient (primarily nitrogen and phosphorus) inputs from human sources. Estuaries, bays and nearshore coastal waters in the Gulf of Maine receive nutrient inputs from land-based sources via rivers and streams, dir...

  5. 77 FR 56749 - Gulf Coast Ecosystem Restoration

    Science.gov (United States)

    2012-09-13

    ... plan for addressing ecological concerns in the Gulf of Mexico. In light of the release of the Strategy..., including section 311 of the Federal Water Pollution Control Act (FWPCA) (33 U.S.C. 1321), section 1006 of the Oil Pollution Act of 1990 (33 U.S.C. 2706), and section 301 of title 3, United States Code, it...

  6. Rickettsiae in Gulf Coast Ticks, Arkansas, USA

    OpenAIRE

    Trout, Rebecca; Steelman, C Dayton; Szalanski, Allen L.; Williamson, Phillip C

    2010-01-01

    To determine the cause of spotted fever cases in the southern United States, we screened Gulf Coast ticks (Amblyomma maculatum) collected in Arkansas for rickettsiae. Of the screened ticks, 30% had PCR amplicons consistent with Rickettsia parkeri or Candidatus Rickettsia amblyommii.

  7. New offshore platform in the Mexican Gulf

    Energy Technology Data Exchange (ETDEWEB)

    Beisel, T.

    1982-04-01

    After a construction period of only 10 months, the second steel Offshore platform was recently completed in the Mexican Gulf. The pattern for this structure was the Cognac platform. The erection of the new platform, called the 'Cerveza' platform, is described in the article.

  8. Fishery potential of the Gulf of Kachchh

    Digital Repository Service at National Institute of Oceanography (India)

    Nair, V.R.; Govindan, K.; Ramaiah, Neelam; Gajbhiye, S.N.

    /h) was three times more productive than the creek (av. 2.3 kg/h). The number of species found in the Gulf and creek were respectively 34 and 20 suggesting good biodiversity of the living resources of the area....

  9. Egypt : Gulf of Aqaba Environmental Action Plan

    OpenAIRE

    World Bank; European Union

    2000-01-01

    The intensive development of tourism in the Gulf of Aqaba presents both an opportunity and a dilemma for Egypt. Intensive tourism, if left unmanaged, can inflict irreversible damage on coral reef and desert ecosystems and curtail the area's economic potential. Together with current projections for a rapid expansion of the tourism base in the Aqaba coast, degradation from mounting recreatio...

  10. Sediment transport and fan deposition in the Gulf of Alaska: Effects of transform motion on deep sea sedimentation

    Energy Technology Data Exchange (ETDEWEB)

    Stevenson, A.J.; Bruns, T.R.; Carlson, P.R. (Geological Survey, Palo Alto, CA (USA)); Dobson, M.R. (Univ. of College of Wales, Aberystwyth (Wales))

    1990-06-01

    GLORIA side-scan sonar images and two channel seismic profiles recently collected in the Gulf of Alaska reveal a major site of late Miocene to Recent terrigenous sediment accumulation on the oceanic plate adjacent to the Fairweather-Queen Charlotte transform and the Yakutat Terrane. Sediment moving across this margin has formed several large channel dominated fan systems that blanket the entire gulf and spill westward onto the Tufts Abyssal Plain. The Surveyor Fan, fed by the glaciers of the Yakutat Terrane and insulated from transform sediment source offset by the Terrane, has maintained a single channel course over the entire life of the fan. The Chirikov and Baranof fans receive their sediment supply from glaciofluvial point sources along the SE Alaska margin, separated from the fans by an active transform. The fans show a southward younging of channel ages consistent with the sense of plate motion. Early (late Miocene) deposition within the gulf was limited to the structural basin between the continental margin and the Kodiak-Bowie seamount chain. The geometry of these early depositional systems is poorly known, but available data suggest their channels were oriented NW-SE. Subsequent establishment of a depositional slope between the margin and the seamount chain, coupled with the filling of the basin, led to a reorganization into SW-NE channel systems. The fan bodies of the Gulf of Alaska are members of a distinct class of fans that are characterized by long distributary channels which persist to near the fan limits. This type of fan morphology is most often attributed to a predominantly fine-grained sediment supply. This is difficult to reconcile with the obvious proximal glacial source for much of the sediment supplied to these fans.

  11. First results from the SARDINIA deep seismic cruise on the Western Sardinia and Gulf of Lions conjugate margin pair

    Science.gov (United States)

    Gailler, A.; Klingelhoefer, F.; Beslier, M.; Olivet, J.; Aslanian, D.; Bache, F.; Moulin, M.; Matias, L.; Afilhado, A.; Nouze, H.

    2008-12-01

    The deep North-Western Mediterranean (or Provencal) basin was formed by thinning and rotation of the Corsica-Sardinia block which started 30-20 Ma ago. It is bounded by the Gulf of Lions to the north, the Catalan margin to the west, the Ligurian Sea to the east, and the Valencia Trough to the south-west, in which rifting started at roughly the same time as in the Provencal basin. The basin has a depth of up to 2.8 km and a sedimentary layer thickness of up to 8 km. The central part of the basin is presumed to be underlain by a crust of oceanic nature, while the neighboring Valencia Trough is situated on thinned continental crust. During the SARDINIA cruise of the R/V Atalante in December 2006, three wide-angle seismic profiles were acquired in the Gulf of Lions area and three profiles on the conjugate margin offshore Sardinia. The main goals of the SARDINIA project were to image the deep structure of the conjugate margin pair, to characterize the nature of the crust, detect any exhumed upper mantle materiel and to define the geometry of the basins to better constrain the opening history of the basin. During the cruise, a total of 57 ocean bottom seismometers/hydrophones (OBS/OBH) from Ifremer, the University of Brest and Geomar, Kiel were deployed in the Gulf of Lions region and 47 OBS and OBH offshore Sardinia. The lines perpendicular to the margins were recorded by landstations onshore, thus prolonging the profiles. Tomographic and forward wide-angle seismic models of the deep seismic data from the margin perpendicular profile located in the Gulf of Lions image a sedimentary layer up to 8 km thickness, which is locally strongly disturbed by salt tectonics. They indicate, that crustal thinning in the Gulf of Lions area occurs within a 100 km wide zone. East of this zone of crustal thinning is a zone characterized by high velocities in the lower crust (7.2-7.4 km/s) atypical for either thinned continental or normal oceanic crust. The boundary of this layer

  12. Messinian paleoenvironmental evolution in the lower Guadalquivir Basin (SW Spain) based on benthic foraminifera.

    OpenAIRE

    Pérez-Asensio, J.N.; Aguirre, J.; Schmiedl, G.; Civis Llovera, J.

    2012-01-01

    Benthic foraminiferal assemblages of a drill core from the lower Guadalquivir Basin (northern Gulf of Cádiz, SW Spain) have been analyzed in order to reconstruct the paleoenvironmental evolution in the vicinity of the Betic seaways during the Messinian. The core consists of marine sediments ranging from the latest Tortonian to the early Pliocene. Changes in the abundance of certain marker species, planktonic/benthic ratio (P/B ratio), paleodepth estimated with a transfer function, content of ...

  13. Flow-Through, Low Retention Hydrocarbon Generation in Active Sedimentary Basins

    Science.gov (United States)

    Cathles, L. M.

    2002-12-01

    Hydrocarbons are typically generated when thin (consumption of oil to date, from a 100 x 200 km portion of one basin in a relatively short timespan (about 20 Ma) provides an interesting geologic context for human production and consumption. The rapid venting also has potentially important implications for the fisheries food chain in the northern Gulf of Mexico. The venting rate is fast enough that hydrocarbons could be a significant aquatic food source.

  14. Ocean Carbon and Biogeochemistry Scoping Workshop on Terrestrial and Coastal Carbon Fluxes in the Gulf of Mexico, St. Petersburg, FL

    Science.gov (United States)

    Robbins, L. L.; Coble, P. G.; Clayton, T. D.; Cai, W. J.

    2008-01-01

    Despite their relatively small surface area, ocean margins may have a significant impact on global biogeochemical cycles and, potentially, the global air-sea fluxes of carbon dioxide. Margins are characterized by intense geochemical and biological processing of carbon and other elements and exchange large amounts of matter and energy with the open ocean. The area-specific rates of productivity, biogeochemical cycling, and organic/inorganic matter sequestration are high in coastal margins, with as much as half of the global integrated new production occurring over the continental shelves and slopes (Walsh, 1991; Doney and Hood, 2002; Jahnke, in press). However, the current lack of knowledge and understanding of biogeochemical processes occurring at the ocean margins has left them largely ignored in most of the previous global assessments of the oceanic carbon cycle (Doney and Hood, 2002). A major source of North American and global uncertainty is the Gulf of Mexico, a large semi-enclosed subtropical basin bordered by the United States, Mexico, and Cuba. Like many of the marginal oceans worldwide, the Gulf of Mexico remains largely unsampled and poorly characterized in terms of its air-sea exchange of carbon dioxide and other carbon fluxes. The goal of the workshop was to bring together researchers from multiple disciplines studying terrestrial, aquatic, and marine ecosystems to discuss the state of knowledge in carbon fluxes in the Gulf of Mexico, data gaps, and overarching questions in the Gulf of Mexico system. The discussions at the workshop were intended to stimulate integrated studies of marine and terrestrial biogeochemical cycles and associated ecosystems that will help to establish the role of the Gulf of Mexico in the carbon cycle and how it might evolve in the face of environmental change.

  15. The progress in knowledge of physical oceanography of the Gulf of Finland: a review for 1997-2007

    Directory of Open Access Journals (Sweden)

    Tarmo Soomere

    2008-09-01

    Full Text Available The main findings of studies of the physical oceanography of the Gulf of Finland (GoF during 1997-2007 are reviewed. The aim is to discuss relevant updates published in international peer-reviewed research papers and monographs, bearing in mind that a comprehensive overview of the studies up to the mid-1990s is available (Alenius et al. 1998. We start the discussion with updates on the basic hydrographical and stratification conditions, and progress in the understanding of atmospheric forcing and air-sea interaction. Advances in the knowledge of basin-scale and mesoscale dynamics are summarised next. Progress in circulation and water exchange dynamics has been achieved mostly by means of numerical studies. While the basic properties of circulation patterns in the gulf have been known for a century, new characteristics and tools such as water age, renewal index, and high-resolution simulations have substantially enriched our knowledge of processes in the Gulf of Finland during the last decade. We present the first overview of both status and advances in optical studies in this area. Awareness in this discipline has been significantly improved as a result of in situ measurements. Our understanding of the short- and long-term behaviour of the sea level as well as knowledge of the properties of both naturally and anthropogenically induced surface waves have expanded considerably during these ten years. Developments in understanding the ice conditions of the Gulf of Finland complete the overview, together with a short discussion of the gulf's future, including the response to climate change. Suggestions for future work are outlined.

  16. The Mimallonidae (Lepidoptera, Mimallonoidea) of the Caribbean Basin, with the descriptions of two new species.

    Science.gov (United States)

    Laurent, Ryan A St; Mccabe, Timothy L

    2016-01-01

    Mimallonidae of the Caribbean Basin are discussed, with attention primarily given to species endemic to the Caribbean islands and the northern coast of Venezuela. The Caribbean Basin is a political term for tropical regions circumscribed by the Gulf of Mexico. Cicinnus bahamensis sp. n. is described from the Bahamas, the first species of Mimallonidae from this country. The Cuban species Cicinnus packardii (Grote, 1865), the closest relative of C. bahamensis sp. n., is figured and compared. A third, similar, species from northern coastal Venezuela, C. falcoargenteus sp. n., is described and compared to the previous two species. PMID:27394281

  17. Importance of the Mississippi River Basin for investigating agricultural–chemical contamination of the hydrologic cycle

    Science.gov (United States)

    Kolpin, Dana W.

    2000-01-01

    This special issue is devoted to recent and ongoing research relating to the fate and transport of agricultural chemicals in the Mississippi River Basin by the US Geological Survey Toxic Substances Hydrology (Toxics) Program. The Mississippi River Basin drains approximately 3 200 000 km2 representing 41% of the United States. This is the largest river in the United States and the third largest in the world. The Mississippi River discharges an average of 19 920 m3/s of water into the Gulf of Mexico. The river is an extensively used resource, supplying drinking water to 70 cities in the United States.

  18. Deep Structure and Evolution of the Northeastern Gulf of Aden Margin From Wide-Angle Seismic and Thermomechanical Modelling

    OpenAIRE

    Watremez, Louise

    2010-01-01

    The Gulf of Aden is a young oceanic basin which separates Arabian from Somalian plates. The present-day opening velocity is about 2 cm/yr. Continental rifting began at 35 Ma and sea oor spreading at least at 17.6 Ma. The western passive margins, close to the Afar hotspot, are volcanic, while they are non-volcanic in the East. The conjugate margins are relatively young and associated to a thin sedimentary cover ; this makes them easy to correlate. So, the study of the deep structure of the nor...

  19. Mid- to Late Holocene Climate Shift in the Southern Gulf of California and Tropical Pacific Ocean

    Science.gov (United States)

    Perez-Cruz, L. L.; Fucugauchi, J. U.; Velasco, V.; Rodriguez, A.; Choumiline, K.

    2014-12-01

    A multiproxy record has been acquired from a gravity core (DIPAL-I K47) taken in La Paz Basin, an area which is situated in the southwestern sector of the Gulf of California at the junction to the Tropical Pacific Ocean. The high-resolution data sets, from XRF, TOC, magnetic susceptibility and hysteresis measurements, were used to track climatic changes in the tropical climate system at sub-centennial time scales over the past 7.3 cal kyr BP. The paleoprecipitation record shows variation trends, with a shift during the mid- to late Holocene, characterized by changes from high to low humidity. Pluvial, biogenic and eolian input, marked by variations in Ti, Si, Fe, K, Ca, Zr/Ti, Ca/Ti and magnetic susceptibility, shows trend changes between 7-5 cal kyr, 5-4.5 cal kyr, 4.5-3.5 cal kyr and 2.15-1.4 kyr. Drought events are recognized from 3.7 to 3.4, 2.8 to 1.8 cal kyr BP, and between 1.4 and 1.2 cal kyr BP. The southern Gulf is well suited for documenting the climatic and precipitation changes in the tropical Pacific Ocean associated with ITCZ latitudinal migration, PDO, ENSO events and the North American monsoon. Analysis of sourcing, transport and deposition of sediments is used for reconstructing the changing ocean-atmosphere circulation patterns, particularly sensitive to paleoprecipitation. The Bay receives sediments mainly from the surrounding volcanic ranges of the peninsular Baja California. There are no rivers in the peninsula and sediments are related to pluvial input trough ephemeral creeks along the steep cliff ranges and narrow shelf. Biogenic sediments are associated with productivity and oceanographic conditions through upwellings and mesoscale gyres. Eolian sediments are transported into the basin from the peninsula and continent, including transport of fine dust from the northern desert of Sonora-Mojave and arid terrains in the peninsula. It is important to highlight that a common 1800 yr solar variation spectral periodicity has been captured

  20. Depleted uranium and the Gulf War syndrome

    International Nuclear Information System (INIS)

    Some military personnel involved in the 1991Gulf War have complained of continuing stress-like symptoms for which no obvious cause has been found. These symptoms have at times been attributed to the use of depleted uranium (DU) in shell casings which are believed to have caused toxic effects. Depleted uranium is natural uranium which is depleted in the rarer U-235 isotope. It is a heavy metal and in common with other heavy metals is chemically toxic. It is also slightly radioactive and could give rise to a radiological hazard if dispersed in finely divided form so that it was inhaled. In response to concerns, the possible effects of DU have been extensively studied along with other possible contributors to Gulf War sickness. This article looks at the results of some of the research that has been done on DU. (author)

  1. Gulf of Mexico forecasts : the dead sea

    International Nuclear Information System (INIS)

    The future gas supply potential from the offshore Gulf of Mexico region was discussed with particular emphasis on the issue of whether there is enough growth potential to satisfy the anticipated growth in power generation markets. In 1980, a forecasted decrease in gas supply proved to be wrong. In fact, supply actually increased and productivity in the Gulf of Mexico has been relatively stable since 1982. A significant growth has been forecasted for 1997 to 2010. This growth will coincide with a large growth in gas demand in the northeastern U.S. The fact that electric power generation is changing hands adds to the opportunities in the northeast. It was emphasized that Canadian supply must be present to compete. 1 tab., 16 figs

  2. Time required for gulf restoration uncertain

    International Nuclear Information System (INIS)

    Hurricane Andrew's long term effect on Gulf of Mexico oil and gas operations likely won't be known until next year. This paper reports that while damage assessments have moved beyond the emergency stage, many offshore service companies say reliable estimates of the extent of damage or cost of repairs still are unavailable. The time needed to complete restorations won't be known conclusively until more organized surveys are complete. Even then, many contractors say, gulf operators must decide how to handle damage at each location-whether to repair damaged structures or replace them by applying technology not available when many of the fields were developed. Some damaged installations will not be replaced or restored, and the production will be lost

  3. Gulf of Mexico Regional Collaborative Final Report

    Energy Technology Data Exchange (ETDEWEB)

    Judd, Kathleen S. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Judd, Chaeli [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Engel-Cox, Jill A. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Gulbransen, Thomas [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Anderson, Michael G. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Woodruff, Dana L. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Thom, Ronald M. [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Guzy, Michael [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Hardin, Danny [Pacific Northwest National Lab. (PNNL), Richland, WA (United States); Estes, Maury [Pacific Northwest National Lab. (PNNL), Richland, WA (United States)

    2007-12-01

    This report presents the results of the Gulf of Mexico Regional Collaborative (GoMRC), a year-long project funded by NASA. The GoMRC project was organized around end user outreach activities, a science applications team, and a team for information technology (IT) development. Key outcomes are summarized below for each of these areas. End User Outreach; Successfully engaged federal and state end users in project planning and feedback; With end user input, defined needs and system functional requirements; Conducted demonstration to End User Advisory Committee on July 9, 2007 and presented at Gulf of Mexico Alliance (GOMA) meeting of Habitat Identification committee; Conducted significant engagement of other end user groups, such as the National Estuary Programs (NEP), in the Fall of 2007; Established partnership with SERVIR and Harmful Algal Blooms Observing System (HABSOS) programs and initiated plan to extend HABs monitoring and prediction capabilities to the southern Gulf; Established a science and technology working group with Mexican institutions centered in the State of Veracruz. Key team members include the Federal Commission for the Protection Against Sanitary Risks (COFEPRIS), the Ecological Institute (INECOL) a unit of the National Council for science and technology (CONACYT), the Veracruz Aquarium (NOAA’s first international Coastal Ecology Learning Center) and the State of Veracruz. The Mexican Navy (critical to coastal studies in the Southern Gulf) and other national and regional entities have also been engaged; and Training on use of SERVIR portal planned for Fall 2007 in Veracruz, Mexico Science Applications; Worked with regional scientists to produce conceptual models of submerged aquatic vegetation (SAV) ecosystems; Built a logical framework and tool for ontological modeling of SAV and HABs; Created online guidance for SAV restoration planning; Created model runs which link potential future land use trends, runoff and SAV viability; Analyzed SAV

  4. A high-resolution hydrodynamic-biogeochemical coupled model of the Gulf of Cadiz – Alboran Sea region.

    Directory of Open Access Journals (Sweden)

    D. M. MACIAS

    2015-01-01

    Full Text Available The southern Iberia regional seas comprise the Gulf of Cadiz and the Alboran Sea sub-basins connected by the narrow Strait of Gibraltar. Both basins are very different in their hydrological and biological characteristics but are, also, tightly connected to each other. Integrative studies of the whole regional oceanic system are scarce and difficult to perform due to the relative large area to cover and the different relevant time-scales of the main forcings in each sub-basin. Here we propose, for the first time, a fully coupled, 3D, hydrodynamic-biogeochemical model that covers, in a single domain (~2km resolution both marine basins for a 20 years simulation (1989-2008. Model performance is assessed against available data in terms of spatial and temporal distributions of biological variables. In general, the proposed model is able to represent the climatological distributions of primary and secondary producers and also the main seasonality of primary production in the different sub-regions of the analyzed basins. Potential causes of the observed mismatches between model and data are identified and some solutions are proposed for future model development. We conclude that most of these mismatches could be attributed to the missing tidal forcing in the actual model configuration. This model is a first step to obtain a meaningful tool to study past and future oceanographic conditions in this important marine region constituting the unique connection of the Mediterranean Sea with the open world’s ocean.

  5. Natural gamma radionuclides in sediments of Gulf of Mexico: An approach to radio-tracers transport and distribution of sediments in marine environments

    International Nuclear Information System (INIS)

    The following paper contains information of 23 cores collected nuclides in the Gulf of Mexico from 70 to 2,100 meters of depth. The cores were collected in Mexican Gulf of Mexico on OGMEX Oceanographic Campaigns between 1993 and 1995. Radiometric determinations were measured by the Silena gamma-spectrometer from 50 to 60,000 s at the Environmental Laboratory in Cienfuegos, Cuba. A database of 920 natural radio-nuclides from chains of 232Th and 238U, was obtained from 180 samples. The most significant result was the geographic distribution of gamma radionuclides measured concentrations is regionally distinct. Finding a low 238U gamma radio-nuclides concentration at low depth zones and high concentration in depth waters. While the already mentioned conditions are inverted for the 232Th gamma radionuclides. As it is the case of 214Pb and 212Pb. The discussion of results as here presented allows to assume a geographic distribution of natural gamma radionuclides under sedimentary material supplying conditions by the hydrological basins which drain to the Gulf of Mexico and the marine currents transport those materials through the inside of the Gulf of Mexico. Associated results are shown to the rest of Gamma Radionuclides Natural that belong to the 238U and 232Th chains in order to permit corroborating associations in different proportions of these radionuclides in geological material of hydrological basins associated to the western slope in the Gulf of Mexico. In conclusion the work as here presented allows the understanding and elucidation of the origin, transport and, deposition of sedimentary material by means of natural radionuclides tracers using low gamma spectrometry

  6. Natural gamma radionuclides in sediments of the Gulf of Mexico: An approach to radio-tracers transport and distribution of sediments in marine environments

    International Nuclear Information System (INIS)

    The following paper contains information of 23 cores collected nuclides in the Gulf of Mexico from 70 to 2,100 meters of depth. The cores were collected in Mexican Gulf of Mexico on OGMEX Oceanographic Campaigns between 1993 and 1995. Radiometric determinations were measured by the Silena gamma-spectrometer from 50 to 60,000 s at the Environmental Laboratory in Cienfuegos, Cuba. A database of 920 natural radio-nuclides from chains of 232Th and 238U, was obtained from 180 samples. The most significant result was the geographic distribution of gamma radionuclides measured concentrations is regionally distinct. Finding a low 238U gamma radio-nuclides concentration at low depth zones and high concentration in depth waters. While the already mentioned conditions are inverted for the 232Th gamma radionuclides. As it is the case of 214Pb and 212 Pb. The discussion of results as here presented allows to assume a geographic distribution of natural gamma radionuclides under sedimentary material supplying conditions by the hydrological basins which drain to the Gulf of Mexico and the marine currents transport those materials through the inside of the Gulf of Mexico. Associated results are shown to the rest of Gamma Radionuclides Natural that belong to the 238U and 232Th chains in order to permit corroborating associations in different proportions of these radionuclides in geological material of hydrological basins associated to the western slope in the Gulf of Mexico. In conclusion the work as here presented allows the understanding and elucidation of the origin, transport and, deposition of sedimentary material by means of natural radionuclides tracers using low gamma spectrometry

  7. NASA Gulf of Mexico Initiative Hypoxia Research

    Science.gov (United States)

    Armstrong, Curtis D.

    2012-01-01

    The Applied Science & Technology Project Office at Stennis Space Center (SSC) manages NASA's Gulf of Mexico Initiative (GOMI). Addressing short-term crises and long-term issues, GOMI participants seek to understand the environment using remote sensing, in-situ observations, laboratory analyses, field observations and computational models. New capabilities are transferred to end-users to help them make informed decisions. Some GOMI activities of interest to the hypoxia research community are highlighted.

  8. Q&A on Beibu Gulf

    Institute of Scientific and Technical Information of China (English)

    Alice

    2010-01-01

    China-ASEAN FTA, the world's largest free trade area in terms of population took effect on January 1, 2010, covering 13 million square kilometers and 1.9 billion people. Over 90 percent of the commodities traded between China and the six original ASEAN countries, including Brunei, Indonesia, Malaysia, the Philippines, Singapore and Thailand, now enjoy no tariffs from 2010. As a window to ASEAN countries, Beibu Gulf Economic Zone is in more limelight since the new year.

  9. Upwelling in the Gulf of Lions

    OpenAIRE

    Millot, Claude; Wald, Lucien

    1981-01-01

    International audience The hydrological and meteorological characteristics of the Gulf of Lions are such that upwelling occurs with no bias due to tides or strong longshore circulation. The sky is generally cloud-free, an uncommon feature in an upwelling area that allows extensive use of satellite infrared data. The observations are adequate to compute mean maps of the sea-surface temperature during upwelling events. Undoubtedly upwelling is much more intense along straitght coastal segmen...

  10. Gulf of Antalya, Southern Turkish Coastline

    Science.gov (United States)

    1984-01-01

    The historic and strategic southern Turkish coastline and Gulf of Antalya (37.0N, 31.0E) has, since ancient times, served as the classic land and sea invasion routes to the riches of the Near East as Persian, Greek, Roman and later European Crusader armies traveled the familiar routes of conquest. Even in modern times, this area is still the seat of political and military unrest as diverse cultural groups still strive for regional control.

  11. Gulf of Mexico mud toxicity limitations

    Energy Technology Data Exchange (ETDEWEB)

    Dunn, H.E.; Beardmore, D.H. (Phillips Petroleum Co., Bartlesville, OK (USA)); Stewart, W.S. (Drilling Specialties Co. (US))

    1989-10-01

    Because of the Environmental Protection Agency's recent toxicity limits on drilling mud discharges for offshore Gulf of Mexico, Phillips Petroleum conducted a mud toxicity study based on both field and lab tests. The study, discussed in this article, found the polyanionic cellulose-sulfomethylated quebracho-chrome lignosulfonate mud Phillips had been using would comfortably pass the toxicity limitations. The study also found barite and thinners were of low toxicity, and hydrocarbons and surfactants were highly toxic.

  12. 77 FR 39998 - Gulf of Mexico Fishery Management Council; Public Meeting

    Science.gov (United States)

    2012-07-06

    ...The Gulf of Mexico Fishery Management Council (Council) will convene its Law Enforcement Advisory Panel (LEAP) in conjunction with the Gulf States Marine Fisheries Commission's Law Enforcement Committee...

  13. Prey consumption and energy transfer by marine birds in the Gulf of Alaska

    Science.gov (United States)

    Hunt, G.L., Jr.; Drew, G.S.; Jahncke, J.; Piatt, J.F.

    2005-01-01

    We investigated prey consumption by marine birds and their contribution to cross-shelf fluxes in the northern Gulf of Alaska. We utilized data from the North Pacific Pelagic Seabird Database for modeling energy demand and prey consumption. We found that prey consumption by marine birds was much greater over the continental shelf than it was over the basin. Over the shelf, subsurface-foraging marine birds dominated food consumption, whereas over the basin, surface-foraging birds took the most prey biomass. Daily consumption by marine birds during the non-breeding season ("winter") from September through April was greater than daily consumption during the breeding season, between May and August. Over the shelf, shearwaters, murres and, in winter, sea ducks, were the most important consumers. Over the basin, northern fulmars, gulls and kittiwakes predominated in winter and storm-petrels dominated in May to August. Our results suggest that marine birds contribute little to cross-shelf fluxes of energy or matter, but they do remove energy from the marine system through consumption, respiration and migration. ?? 2005 Elsevier Ltd. All rights reserved.

  14. Sediment Sources in the Persian Gulf

    Science.gov (United States)

    Mahoutian, Mehrab

    2014-05-01

    Sediment Constituent Analysis is an effective tool for identifying sediment sources. Based on several sediment samples taken from different sites all over the Iranian coastlines, we have been able to show that an important portion of sediment on the beaches in the Persian Gulf is bio-clastic; that is, biologically created from the coral environment as well as other marine habitats. Unlike mineral (clastic) sediments, carbonate sediments are born not made. Furthermore, carbonate sand constituents are generally less durable than their quartz and mineral counterparts, and break down relatively quickly. Therefore, destruction of reefs and degradation of marine habitat are certain to reduce the sand supply to the shoreline in the Persian Gulf that is necessary to maintain beaches. Carbonate sands are also found on the coastline of the Oman Sea. One of the striking things about the sediments along the coastline of Iran is the high percentage of carbonate material. Molluscan debris is common, even ubiquitous. This reflects the populations living in the offshore waters. Some molluscs thrive in high-energy sandy environments, others like finer sediments. Some live at the surface, while some burrow down as much as a half-metre. A great deal of information can be gained from the study of the species of mollusk and their distribution in the sediments. This paper introduces a few case studies done in different parts of the Persian Gulf by using this method as a general assessment toolbox.

  15. 78 FR 76758 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2013-12-19

    ...NMFS announces the closure date of the recreational season for red snapper in the exclusive economic zone (EEZ) of the Gulf of Mexico (Gulf) for the 2014 fishing season through this temporary rule. Federal waters of the Gulf will close to red snapper recreational harvest at 12:01 a.m., July 11, 2014. This closure is necessary to prevent the recreational sector from exceeding its quota for the......

  16. Estimating tsunami inundation from hurricane storm surge predictions along the U.S. gulf coast

    Science.gov (United States)

    Pampell-Manis, Alyssa; Horrillo, Juan; Figlus, Jens

    2016-06-01

    Gulf of Mexico (GOM) coasts have been included in the U.S. Tsunami Warning System since 2005. While the tsunami risk for the GOM is low, tsunamis generated by local submarine landslides pose the greatest potential threat, as evidenced by several large ancient submarine mass failures identified in the northern GOM basin. Given the lack of significant historical tsunami evidence in the GOM, the potential threat of landslide tsunamis in this region is assessed from a worst-case scenario perspective based on a set of events including the large ancient failures and most likely extreme events determined by a probabilistic approach. Since tsunamis are not well-understood along the Gulf Coast, we investigate tsunami inundation referenced to category-specific hurricane storm surge levels, which are relatively well established along the Gulf Coast, in order to provide information for assessing the potential threat of tsunamis which is more understandable and accessible to emergency managers. Based on tsunami inundation studies prepared for the communities of South Padre Island, TX, Galveston, TX, Mobile, AL, Panama City, FL, and Tampa, FL, we identify regional trends of tsunami inundation in terms of modeled storm surge inundation. The general trends indicate that tsunami inundation can well exceed the level of storm surge from major hurricanes in open beachfront and barrier island regions, while more interior areas are less threatened. Such information can be used to better prepare for tsunami events as well as provide a preliminary estimate of tsunami hazard in locations where detailed tsunami inundation studies have not been completed.

  17. Environmental Assessment: Geothermal Energy Geopressure Subprogram. Gulf Coast Well Testing Activity, Frio Formation, Texas and Louisiana

    Energy Technology Data Exchange (ETDEWEB)

    None

    1978-02-01

    This Environmental Assessment (EA) has been prepared to provide the environmental input into the Division of Geothermal Energy's decisions to expand the geothermal well testing activities to include sites in the Frio Formation of Texas and Louisiana. It is proposed that drilling rigs be leased before they are removed from sites in the formation where drilling for gas or oil exploration has been unsuccessful and that the rigs be used to complete the drilling into the geopressured zone for resource exploration. This EA addresses, on a regional basis, the expected activities, affected environment, and the possible impacts in a broad sense as they apply to the Gulf Coast well testing activity of the Geothermal Energy Geopressure Subprogram of the Department of Energy. Along the Texas and Louisiana Gulf Coast (Plate 1 and Overlay, Atlas) water at high temperatures and high pressures is trapped within Gulf basin sediments. The water is confined within or below essentially impermeable shale sequences and carries most or all of the overburden pressure. Such zones are referred to as geopressured strata. These fluids and sediments are heated to abnormally high temperatures (up to 260 C) and may provide potential reservoirs for economical production of geothermal energy. The obvious need in resource development is to assess the resource. Ongoing studies to define large-sand-volume reservoirs will ultimately define optimum sites for drilling special large diameter wells to perform large volume flow production tests. in the interim, existing well tests need to be made to help define and assess the resource.

  18. Melo carboniferous basin

    International Nuclear Information System (INIS)

    This report is about of the Melo carboniferous basin which limits are: in the South the large and high Tupambae hill, in the west the Paraiso hill and the river mountains, in the North Yaguaron river basin to Candidata in Rio Grande del Sur in Brazil.

  19. Transtensional Rifting in the Late Proto-Gulf of California Near Bahía Kino, Sonora, México

    Science.gov (United States)

    Bennett, S. E.; Oskin, M. E.; Dorsey, R. J.

    2009-12-01

    We investigate the role of obliquity in continental rupture from the example of the Gulf of California rift. Focused transtensional strain adjacent to strike-slip faults, ubiquitous in oblique rifts, may act as a catalyst for lithospheric rupture. To test this hypothesis we completed detailed structural mapping, fault kinematic analysis, basin analysis, and paleomagnetism of pre- and syn-rift volcanic and sedimentary rocks exposed in coastal Sonora, near Bahía Kino, México. This area is host to the NW-striking, dextral Sacrificio and Bahía Kino faults onshore that are likely linked to the offshore De Mar transform fault that accommodated Gulf opening. Three fault-bounded sedimentary basins formed unconformably above the 12.50 ± 0.08 Ma Tuff of San Felipe. The 6.53 ± 0.18 Ma Tuff of Cerro Tordillo and the 6.39 ± 0.02 Ma Tuffs of Mesa Cuadrada are interbedded in the lower part of the non-marine basin fill. In one of these basins, we used these tuff markers to calibrate a sedimentation rate of 1.2 ± 0.2 mm/yr and a tilting rate of 0.12 ± 0.02 °/kyr. These rapid rates suggest transtensional strain and related basin subsidence initiated ca. 6.6 Ma, near the end of proto-Gulf time. Paleomagnetism of the Tuff of San Felipe and Tuffs of Mesa Cuadrada in coastal Sonora show variable amounts of clockwise vertical-axis rotation when compared to paleomagnetic reference sites in Baja California. Fault blocks in the central and southern parts of the study area are rotated counter-clockwise 15° to clockwise 35°. Strike-slip faults in this area accommodate up to 10 km of slip. In contrast, ~53° of clockwise rotation occurred in the northern part of the study area, where strike-slip faults are absent. In this northern area, transtensional deformation occurred primarily by block rotation and ~6 km of normal slip on the low-angle (5-15°) Punta Chueca fault. After correcting for variable amounts of rotation, fault blocks display a consistent tilt down to the ENE. Pre

  20. Attributes for NHDPlus Catchments (Version 1.1): Basin Characteristics, 2002

    Science.gov (United States)

    Wieczorek, Michael E.; LaMotte, Andrew E.

    2010-01-01

    This data set represents basin characteristics, compiled for every catchment in NHDPlus for the conterminous United States. These characteristics are basin shape index, stream density, sinuosity, mean elevation, mean slope, and number of road-stream crossings. The source data sets are the U.S. Environmental Protection Agency's NHDPlus and the U.S. Census Bureau's TIGER/Line Files. The NHDPlus Version 1.1 is an integrated suite of application-ready geospatial datasets that incorporates many of the best features of the National Hydrography Dataset (NHD) and the National Elevation Dataset (NED). The NHDPlus includes a stream network (based on the 1:100,00-scale NHD), improved networking, naming, and value-added attributes (VAAs). NHDPlus also includes elevation-derived catchments (drainage areas) produced using a drainage enforcement technique first widely used in New England, and thus referred to as "the New England Method." This technique involves "burning in" the 1:100,000-scale NHD and when available building "walls" using the National Watershed Boundary Dataset (WBD). The resulting modified digital elevation model (HydroDEM) is used to produce hydrologic derivatives that agree with the NHD and WBD. Over the past two years, an interdisciplinary team from the U.S. Geological Survey (USGS), and the U.S. Environmental Protection Agency (USEPA), and contractors, found that this method produces the best quality NHD catchments using an automated process (USEPA, 2007). The NHDPlus dataset is organized by 18 Production Units that cover the conterminous United States. The NHDPlus version 1.1 data are grouped by the U.S. Geologic Survey's Major River Basins (MRBs, Crawford and others, 2006). MRB1, covering the New England and Mid-Atlantic River basins, contains NHDPlus Production Units 1 and 2. MRB2, covering the South Atlantic-Gulf and Tennessee River basins, contains NHDPlus Production Units 3 and 6. MRB3, covering the Great Lakes, Ohio, Upper Mississippi, and Souris

  1. A Geographic Information System (GIS) analysis for trace metal assessment of sediments in the Gulf of Paria, Trinidad

    International Nuclear Information System (INIS)

    The Gulf of Paria is a semi-enclosed shallow basin with increasing coastal development activities along Trinidad's west coast. Sediments present a host for trace metal pollutants from overlying waters, therefore determination of their content is critical in evaluating and detecting sources of marine pollution. This paper presents a Geographic Information System (GIS) analysis of geochemical assessment for trace metals in coastal sediments of the Gulf of Paria. This GIS approach facilitates interpretation of the spatial relationships among key environmental processes. The GIS development involves the integration of spatial and attribute data pertaining to bathymetry, current systems, topography, rivers, land use/land cover and coastal sediments. It employs spatial interpolation and retrieval operations to analyze the total trace metal concentrations of aluminum, copper and lead in the sediments and the clay-enriched sediments, to determine whether they are related to sediment type or are affected by the discharge from anthropogenic sources. Spatial distribution modeling of element concentrations are produced to indicate contamination plumes from possible anthropogenic sources such as rivers entering the Gulf of Paria, and to reveal potential hot spots and dispersion patterns. A direct spatial correlation between clay-enriched sediments and high concentrations of aluminum and lead is detected, however regions of high concentrations of copper and lead indicate a relationship to anthropogenic sources. The effectiveness of GIS for visualization, spatial query and overlay of geochemical analysis is demonstrated

  2. K Basin safety analysis

    International Nuclear Information System (INIS)

    The purpose of this accident safety analysis is to document in detail, analyses whose results were reported in summary form in the K Basins Safety Analysis Report WHC-SD-SNF-SAR-001. The safety analysis addressed the potential for release of radioactive and non-radioactive hazardous material located in the K Basins and their supporting facilities. The safety analysis covers the hazards associated with normal K Basin fuel storage and handling operations, fuel encapsulation, sludge encapsulation, and canister clean-up and disposal. After a review of the Criticality Safety Evaluation of the K Basin activities, the following postulated events were evaluated: Crane failure and casks dropped into loadout pit; Design basis earthquake; Hypothetical loss of basin water accident analysis; Combustion of uranium fuel following dryout; Crane failure and cask dropped onto floor of transfer area; Spent ion exchange shipment for burial; Hydrogen deflagration in ion exchange modules and filters; Release of Chlorine; Power availability and reliability; and Ashfall

  3. K Basin safety analysis

    Energy Technology Data Exchange (ETDEWEB)

    Porten, D.R.; Crowe, R.D.

    1994-12-16

    The purpose of this accident safety analysis is to document in detail, analyses whose results were reported in summary form in the K Basins Safety Analysis Report WHC-SD-SNF-SAR-001. The safety analysis addressed the potential for release of radioactive and non-radioactive hazardous material located in the K Basins and their supporting facilities. The safety analysis covers the hazards associated with normal K Basin fuel storage and handling operations, fuel encapsulation, sludge encapsulation, and canister clean-up and disposal. After a review of the Criticality Safety Evaluation of the K Basin activities, the following postulated events were evaluated: Crane failure and casks dropped into loadout pit; Design basis earthquake; Hypothetical loss of basin water accident analysis; Combustion of uranium fuel following dryout; Crane failure and cask dropped onto floor of transfer area; Spent ion exchange shipment for burial; Hydrogen deflagration in ion exchange modules and filters; Release of Chlorine; Power availability and reliability; and Ashfall.

  4. The Gulf of Cádiz pelagic ecosystem: A review

    Science.gov (United States)

    García Lafuente, Jesús; Ruiz, Javier

    2007-08-01

    The Gulf of Cádiz, strategically situated between the North Atlantic Ocean and the Mediterranean Sea, has been the focus of attention of a few oceanographic studies dealing with the deep circulation in order to understand the dynamics of the dense plume of Mediterranean water. Much less attention has been paid to the surface pelagic layer which holds important living resources of commercial and ecological interest. This overview summarizes the recent advances that have been made concerning the regional oceanography of the northern half of this important basin from an interdisciplinary point of view. Probably the most relevant oceanographic feature of the basin is its strong seasonality, which is linked to the meteorologically-induced seasonality of the eastern boundary current system of the North Atlantic. The prominent cape Santa Maria divides the continental shelf off the southern Iberian Peninsula in two shelves of different shape that hold different oceanographic processes, which in turn determine the characteristics of the pelagic ecosystem. Mass and energy inputs from land as well as tidally-driven processes makes the wider eastern shelf be more productive while the narrower western shelf, cut by a sharp submarine canyon, is under the influence of the almost-permanent upwelling spot off cape San Vicente. Under easterlies, the west-going, warm coastal countercurrent that is observed in the eastern shelf may invade the western shelf thus connecting biologically both shelves in an east-to-west direction. Westerlies induce generalised upwelling off the southern Iberia Peninsula, which adds to the almost-permanent one off cape San Vicente and generates an upwelling jet that moves eastwards. Cape Santa Maria may deflect this flow by generating a cold filament that extends southward and diverts water from the western shelf to the open ocean. This pattern of circulation hampers the biological connection between shelves in the west-to-east direction, which is

  5. Structural evolution of the southern transfer zone of the Gulf of Suez rift, Egypt

    Science.gov (United States)

    Abd-Allah, Ali M. A.; Abdel Aal, Mohamed H.; El-Said, Mohamed M.; Abd El-Naby, Ahmed

    2014-08-01

    We present a detailed study about the initiation and reactivations of Zeit-El Tor transfer zone, south Gulf of Suez rift, and its structural setting and tectonic evolution with respect to the Cretaceous-Cenozoic tectonic movements in North Egyptian margin. NE trending zone of opposed-dipping faults (22 km wide) has transferred the NE and SW rotations of the sub-basins in central and south Gulf of Suez rift, respectively. The evolution of this zone started by reactivation of the NE oriented late Neoproterozoic fractures that controlled the occurrence of Dokhan Volcanics in the rift shoulders. Later, the Syrian Arc contraction reactivated these fractures by a sinistral transpression during the Late Cretaceous-Eocene time. N64°E extension of the Oligo-Miocene rift reactivated the NE fractures by a sinistral transtension. During this rifting, the NE trending faults forming the transfer zone were more active than the rift-bounding faults; the Upper Cretaceous reverse faults in the blocks lying between these NE trending faults were rotated; and drape-related reverse faults and the positive flower structures were formed. Tectonic inversion from contraction to extension controlled the distribution and thickness of the Upper Cretaceous-Miocene rocks.

  6. Digitization of a geologic map for the Quebec-Maine-Gulf of Maine global geoscience transect

    Science.gov (United States)

    Wright, Bruce E.; Stewart, David B.

    1990-01-01

    The Bedrock Geologic Map of Maine was digitized and combined with digital geologic data for Quebec and the Gulf of Maine for the Quebec-Maine-Gulf of Maine Geologic Transect Project. This map is being combined with digital geophysical data to produce three-dimensional depictions of the subsurface geology and to produce cross sections of the Earth's crust. It is an essential component of a transect that stretches from the craton near Quebec City, Quebec, to the Atlantic Ocean Basin south of Georges Bank. The transect is part of the Global Geosciences Transect Project of the International Lithosphere Program. The Digital Line Graph format is used for storage of the digitized data. A coding scheme similar to that used for base category planimetric data was developed to assign numeric codes to the digitized geologic data. These codes were used to assign attributes to polygon and line features to describe rock type, age, name, tectonic setting of original deposition, mineralogy, and composition of igneous plutonic rocks, as well as faults and other linear features. The digital geologic data can be readily edited, rescaled, and reprojected. The attribute codes allow generalization and selective retrieval of the geologic features. The codes allow assignment of map colors based on age, lithology, or other attribute. The Digital Line Graph format is a general transfer format that is supported by many software vendors and is easily transferred between systems.

  7. Seismic-stratigraphic geochemical model of occurrence of oils in Gulf of Mexico flexure trend

    Energy Technology Data Exchange (ETDEWEB)

    Dinkelman, M.; Curry, D.J.

    1988-01-01

    Several models have recently been proposed for the generation and migration of the oil and gas in the Gulf of Mexico flexure trend. However, geologic and geochemical data suggest that much of the flexure trend oil was generated in Cretaceous-upper Tertiary sediments and migrated vertically through the faulting associated with continued salt tectonism. Generalized cross sections along the continental margin commonly show a thick, continuous salt layer. Regional seismic stratigraphic analysis shows that the salt is discontinuous in many places along the middle and lower slope owing to thinning and perforation caused by basinward creep, withdrawal, diapirism, and tonguing. The discontinuous salt distribution allows direct stratigraphic contact in places between the late Tertiary sediments and the underlying Paleogene and Cretaceous intervals. Seismic data indicate the salt movement has captured large volumes of slope and basinal sediments through ridging and tonguing. The onset of significant sediment loading on the shelf during the mid-Miocene to Pleistocene implies that shelf instability and sediment capture did not commence until the late Miocene. This scenario is consistent with geochemical data indicating that flexure trend oils are probably from carbonate-rich sources deposited in relatively shallow water. In contrast, Neogene sediments in the Gulf are clastic in nature, and were deposited in environments unfavorable for the accumulation of oil-prone organic matter. Mature migrated bitumens from carbonate sections recovered at DSDP Sites 535 and 540 are very similar geochemically to flexure trend oils.

  8. No evidence for altered cellular immune functions in personnel deployed in the Persian Gulf during and after the Gulf War--The Danish Gulf War study

    DEFF Research Database (Denmark)

    Bregenholt, S; Ishøy, T; Skovgaard, L T;

    2001-01-01

    analyzed the peripheral blood natural killer (NK) cell activity of 686 Gulf War personnel who had been present in the Persian Gulf area during and immediately after the Gulf War as well as 231 gender and age-matched controls. The test material included individual samples of frozen peripheral blood...... mononuclear cells kept at -139 degrees C for a period of 50 to 380 days prior to NK cell analysis of freshly thawed cells. Significant differences in NK-cell activity were not observed by direct comparison of the levels of natural cytotoxic activity in the two groups. However, NK-cell cytotoxicity as such...

  9. New Constraints on the Timing, Magnitude and Style of Deformation in the Southern Gulf of California: Oblique Rifting Since ~14-12 Ma

    Science.gov (United States)

    Kent, G. M.; Harding, A. J.; Sutherland, F. H.; Umhoefer, P. J.; Lizarralde, D.; Driscoll, N. W.

    2008-12-01

    A multichannel seismic (MCS) profile spanning 600 km across conjugate rifted margins in the southern Gulf of California provides insight into the spatial and temporal evolution of extension of the Baja peninsula away from mainland Mexico. Stratigraphic analysis of multiple rifted basins within the Alarcon spreading corridor indicates an initial stage of extension starting near or shortly after 14-12 Ma. This initial phase of extension was characterized by the formation of several large, widely distributed basins, that show little to no syn-rift sedimentation. A second phase of extension, likely synchronous with large-scale basin opening in the central and northern Gulf of California, began at or near 6 Ma, and was characterized by the formation of smaller half-grabens along both conjugate margins, with syn- and post-rift sedimentary sequences. A key feature imaged in the MCS data is a highly reflective, ropey layer at the top of basement with a maximum thickness variation ranging between 250-500 m. Travel-time modeling of common mid-point (CMP) supergathers shows that this layer has a P-wave velocity of around 2.5 km/s, overlying a basement velocity of 4 km/s. The ropey reflectivity patterns along with its low P-wave velocity suggests a volcanic origin, which is interpreted to be either late-stage Comondu volcano-clastics ending near 11 Ma, and/or early rifting volcanics that range in age between 10-9 Ma. This layer is imaged continuously over the Tamayo bank and appears to be mantling the Tamayo trough, partially concealing the largest episode of rift-induced subsidence. Basic extrapolation of sediment thickness to time of deposition within the largest basins in this corridor (i.e., Tamayo trough) suggests that the onset of rifting began at ~14-11 Ma. These new spatial and temporal constraints, when combined with a crustal thickness tomographic profile obtained across the entire Alarcon corridor, support a model of NW-SE oblique extension within the Gulf of

  10. Time series current meter data from buoys in the North Atlantic as part of the Deep Circulation in the Gulf of Maine Field Program from platforms GYRE and MARY LOUISE between July 25th, 1985 and August 2nd, 1987 (NODC Accession 0053940)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — A two-year field study to investigate the deep flow between the major basins in the Gulf of Maine. This deep flow of warm-salty Slope water is an important driving...

  11. Geodynamics of the Gulf of California from surface wave tomography

    NARCIS (Netherlands)

    Zhang, X.; Paulssen, H.

    2012-01-01

    The Gulf of California, which forms part of the Pacific-North American plate boundary, is an ideal place to investigate upper mantle dynamics in a continental rifting area. With 19 seismic stations located around the gulf, the NARS-Baja experiment (2002-2008) was designed to image its crustal and ma

  12. Physical processes in the Gulf of Kachchh: A review

    Digital Repository Service at National Institute of Oceanography (India)

    Vethamony, P.; Babu, M.T.

    A brief review of various physical processes acting in the Gulf of Kachchh (GoK), which have prominent roles in Gulf dynamics, is presented in this article. The eddies present in the GoK confirm that they are permanent features of the Go...

  13. 75 FR 16577 - Gulf War Veterans' Illnesses Task Force

    Science.gov (United States)

    2010-04-01

    ... AFFAIRS Gulf War Veterans' Illnesses Task Force AGENCY: Department of Veterans Affairs (VA). ACTION... the Gulf War Veterans' Illnesses Task Force (GWVI-TF) in August 2009 to conduct a comprehensive review... Veterans' Illnesses Task Force Draft Written Report is now complete. The VA is inviting public comments...

  14. Seasonal surface connectivity in the Gulf of California

    Science.gov (United States)

    Marinone, S. G.

    2012-03-01

    A three-dimensional numerical model is used to study seasonal connectivity in the Gulf of California. From the Eulerian velocity fields of the model, particle trajectories were calculated for the 12 months of the year using an advection/diffusion scheme. Connectivity was quantified for twelve Gulf provinces with different dynamic/circulation characteristics being defined by the Eulerian velocity field: strong or weak coastal currents, eddies, and areas of mixing and exchange. Retention occurred for 9-12 months of the year in the Upper Gulf, Eddy and Sonora regions of the northern Gulf because of the Gulf-wide eddy circulation, which implies high potential for the auto-recruitment of larvae in this province. High retention was also found on the peninsula side of the southern Gulf in association with weaker residual currents, again implying potential for self-recruitment. In contrast, low retention was observed on the mainland side of the central and southern Gulf, from which particles are exported to many areas by the faster residual currents enhancing the potential for recruitment of distant coastal species. Empirical Orthogonal Function analyses revealed a strong annual and semiannual evolution in accordance with the strong seasonality of the Gulf dynamics.

  15. Regional Industry Workforce Development: The Gulf Coast Petrochemical Information Network

    Science.gov (United States)

    Hodgin, Johnette; Muha, Susan

    2008-01-01

    The Gulf Coast Petrochemical Information Network (GC-PIN) is a workforce development partnership among industry businesses and area institutions of higher education in the four-county Gulf Coast region. GC-PIN partners develop new industry-specific curricula, foster industry career awareness, and retrain existing employees in new technologies.

  16. Behavior and trends for Zn in Saronikos Gulf

    Directory of Open Access Journals (Sweden)

    Chalkiadakis O.

    2013-04-01

    Full Text Available The study of Zn in the water column of Saronikos Gulf in Greece during a two year period between 2008 and 2010 added data to the available time series of metal data for this marine area since 1985. The Saronikos Gulf, is directly influenced by the Athens metropolitan area. The operation of the Wastewater Treatment Plant of Athens situated on the small island of Psitalia, in 1995, was considered to be the turning point in the efforts of de-pollution of the gulf. Major sources of pollution for the gulf include also the port of Piraeus, with intensive navigation and shipping activities and the significant industrial activity occurring along the coast of Attica. This study of dissolved and particulate Zn gave results consistent with previous studies of the area such as the prevalence of the dissolved form of Zn and the most affected areas being the smaller most enclosed Gulf of Elefsina and Psitalia Island near the wastewater outfall. However, the concentrations of Zn were below toxic levels for marine aquatic organisms. Furthermore, a clear decrease in the Eastern part of the gulf was exhibited as well as a more subtle decrease in the gulf of Elefsina. The levels of Zn in Saronikos Gulf were found comparable to those of other Greek coastal areas.

  17. Gulf Stream eddies - Recent observations in the western Sargasso Sea.

    Science.gov (United States)

    Richardson, P. L.; Knauss, J. A.; Strong, A. E.

    1973-01-01

    A cyclonic Gulf Stream eddy was observed in the western Sargasso Sea by satellite infrared measurements and later confirmed by ship measurements. Fourteen months of observations indicate that the eddy moved southwestward at an average rate of 1 mile per day. The evidence suggests that the eddy was absorbed by the Gulf Stream off Florida.

  18. Who Benefits from Foreign Universities in the Arab Gulf States?

    Science.gov (United States)

    Wilkins, Stephen

    2011-01-01

    The Arab Gulf States are the largest hosts of international branch campuses globally. By increasing higher education capacity in the Arab Gulf States by over 30,000 places, foreign institutions have, through various forms of transnational provision, increased significantly the accessibility of higher education to young people living in these…

  19. Wada basin boundaries and basin cells

    NARCIS (Netherlands)

    Nusse, H.E.; Yorke, J.A.

    1996-01-01

    In dynamical systems examples are common in which two or more attractors coexist, and in such cases the basin boundary is nonempty. We consider a two-dimensional diffeomorphism F (that is, F is an invertible map and both F and its inverse are differentiable with continuous derivatives), which has at

  20. NASA Earth Observations Track the Gulf Oil Spill

    Science.gov (United States)

    Jones, Jason B.; Childs, Lauren

    2010-01-01

    The NASA Applied Sciences Program created the Gulf of Mexico Initiative (GOMI) in 2007 "to enhance the region s ability to recover from the devastating hurricanes of 2005 and to address its coastal management issues going into the future." The GOMI utilizes NASA Earth science assets to address regional priorities defined by the Gulf of Mexico Alliance, a partnership formed by the states of Alabama, Florida, Louisiana, Mississippi, and Texas, along with 13 federal agencies and 4 regional organizations to promote regional collaboration and enhance the ecological and economic health of the Gulf of Mexico. NASA's GOMI is managed by the Applied Science and Technology Project Office at Stennis Space Center and has awarded over $18 million in Gulf of Mexico research since 2008. After the Deepwater Horizon oil spill, GOMI personnel assisted members of the Gulf of Mexico Alliance with obtaining NASA remote sensing data for use in their oil spill response efforts.

  1. Western Gulf of Mexico lease sale draws weak response

    International Nuclear Information System (INIS)

    This paper reports that puny participation in the federal lease sale for the western Gulf of Mexico reflected a lack of open acreage on attractive prospects and the crisis sweeping the U.S. offshore oil and gas industry. Thirty-eight companies participating in the Minerals Management Service's Outer Continental Shelf Sale 141 offered 81 bids for 61 tracts in the western gulf planning area. That was the fewest bids offered in a western gulf sale since operators offered 52 bids for 41 tracts at Sale 105 in August 1986. The only Gulf of Mexico minerals sale to attract less bonus money was the MMS sulfur and salt sale in the central gulf in February 1988 in which $20.8 million was exposed

  2. Three-dimensional flushing times of the Persian Gulf

    Science.gov (United States)

    Sadrinasab, Masoud; Kämpf, Jochen

    2004-12-01

    A three-dimensional hydrodynamic model is employed in a fully prognostic mode to derive flushing times of the Persian Gulf-an evaporation-driven inverse estuary that is governed by import of surface water from the adjacent ocean and export of saline bottom gulf water through the Strait of Hormuz. During spring and summer, a cyclonic overturning circulation establishes along the full length of the Gulf. During autumn and winter, this circulation breaks up into mesoscale eddies, laterally stirring most of the Gulf's surface waters. As a result of this, 95% flushing times of surface waters are shortest (1-3 yr, increasing with distance from the Strait) along the Iranian coast, but are much longer (>5 yr) along the coasts of Kuwait and Saudi Arabia. Owing to density stratification introduced by the surface inflow of ocean water, flushing times of bottom waters are ~6 yr in most parts of the Gulf.

  3. Development of a two-layer mathematical model for the study of hydrodynamic circulation in the sea. Application to the Thermaikos gulf

    Directory of Open Access Journals (Sweden)

    M.G. DODOU

    2012-12-01

    Full Text Available A two-layer hydrodynamic model for stratified flows has been developed and applied to the study of the sea water circulation in the Thermaikos Gulf (North Aegean Sea in the east Mediterranean Sea. The model was based on the finite differences method. The wind and Coriolis forces applied to a stratified basin (with initial density differences ΆΪ/Ϊ = 5ς constituted the basic factors for the study of the circulation in the gulf, corresponding to the stratification conditions. The findings of the model, concerning the basic pattern of circulation in the gulf, were in accordance with in situ data collected in previous studies of the area. Furthermore, the application of the model allowed for the tracking and recognition of the regions of upwelling in the gulf, which were related to the prevailing wind conditions. For the integration of the research, the study was complemented with runs of a two dimensional – depth averaged- model which corresponded to nonstratified conditions. Comparisons and evaluation of the results of the simulations close the study.

  4. The influence of flood basaltic source terrains on the efficiency of tectonic setting discrimination diagrams: An example from the Gulf of Khambhat, western India

    Science.gov (United States)

    Saha, Sourav; Banerjee, Santanu; Burley, Stuart D.; Ghosh, Anupam; Saraswati, Pratul K.

    2010-05-01

    Petrographical and geochemical data of modern coastal and estuarine sediments from the Gulf of Khambhat, western India, illustrate the problem of inferring tectonic setting from petrographic and geochemical discrimination diagrams. The passive margin basin at the western coast of India receives sediments from diverse sources from the stable craton of peninsular India, in which a considerable input is from the Cretaceous Deccan basalt that occupies a major part of the hinterland. Tectonic setting discrimination diagrams do not correctly identify the passive margin signature of sediments from the Gulf of Khambhat in most cases. Tectonic setting is correctly interpreted only in the absence of basaltic derivatives in modern sediments. The sediments predominantly derived from the Deccan basalt are wrongly placed in the oceanic island arc setting in the tectonic discrimination diagrams. Mixing of basaltic sediments derived primarily from the southern rivers with felsic sediments supplied from the northern rivers in the gulf tends to reflect active continental margin and oceanic island to continental island arc settings. Discrimination of the tectonic setting is complicated in estuaries because of the mixing of mafic and felsic derivatives in different proportions. Correct identification of the tectonic setting is possible in the inner estuaries, lying beyond the range of tidal influence, because of negligible mixing of sediments supplied by rivers and by tidal currents. Tectonic setting discrimination diagrams are therefore misleading for modern shallow marine basins situated close to continental flood basalt and, by implication, should be used carefully for ancient successions, given the common occurrence of basalts in the geological record.

  5. Reserves in western basins

    Energy Technology Data Exchange (ETDEWEB)

    Caldwell, R.H.; Cotton, B.W. [Scotia Group, Dallas, TX (United States)

    1995-04-01

    The objective of this project is to investigate the reserves potential of tight gas reservoirs in three Rocky Mountain basins: the Greater Green River (GGRB), Uinta and Piceance basins. The basins contain vast gas resources that have been estimated in the thousands of Tcf hosted in low permeability clastic reservoirs. This study documents the productive characteristics of these tight reservoirs, requantifies gas in place resources, and characterizes the reserves potential of each basin. The purpose of this work is to promote understanding of the resource and to encourage its exploitation by private industry. At this point in time, the GGRB work has been completed and a final report published. Work is well underway in the Uinta and Piceance basins which are being handled concurrently, with reports on these basins being scheduled for the middle of this year. Since the GGRB portion of the project has been completed, this presentation win focus upon that basin. A key conclusion of this study was the subdivision of the resource, based upon economic and technological considerations, into groupings that have distinct properties with regard to potential for future producibility, economics and risk profile.

  6. A Framework for Long-term Monitoring and Research for Agricultural Sustainability in the Lower Mississippi River Basin

    Science.gov (United States)

    Rigby, J.; Locke, M. A.

    2014-12-01

    The Lower Mississippi River Basin (LMRB) is one of the most productive agricultural regions in the United States and has recently become a member of the USDA-ARS Long-term Agricultural Research (LTAR) Network. As the hydrologic gateway to the Gulf of Mexico, the LMRB links agricultural practices and associated runoff and nutrient loads from the Upper Mississippi, Missouri, and Ohio basins with the ecology of the Gulf of Mexico. We review the major challenges for agricultural sustainability in the region and outline a long-term research program within the LTAR Network to address these challenges. Despite the humid climate of the region, water quantity and quality issues are integral to the sustainability of the region. The geography of water-use in the region, current research at plot- to watershed-scales, and knowledge gaps that must be addressed to meet growing production demand will be displayed.

  7. A Paleomagnetic Investigation of Large-Scale Vertical Axis Rotations in Coastal Sonora: Evidence for Transtensional Proto-Gulf Deformation

    Science.gov (United States)

    Herman, S. W.; Gans, P. B.

    2006-12-01

    A paleomagnetic investigation into possible vertical axis rotations has been conducted in the Sierra el Aguaje and Sierra Tinajas del Carmen, Sonora, Mexico, in order assess proposed styles for oblique continental rifting in the Gulf of California. Two styles of rifting have been proposed; (1) strain partitioning (Stock and Hodges, 89), and (2) transtension (Gans, 97), for the Proto-Gulf period of the Gulf of California. The presence of large- scale vertical axis rotations would lend weight to the argument for transtension. The Sierra el Aguaje and Sierra Tinajas del Carmen are located in southwestern coastal Sonora, Mexico. The ranges represent the eastern-rifted margin of the central Gulf of California. This is one of the few areas of that margin which is entirely above water, with new ocean crust of the Guaymas basin lying immediately offshore of the western edge of the ranges. The ranges are composed of volcanic units and their corresponding volcaniclastic units that are the result of persistent magmatic activity between 20 and 8.8 Ma, including three packages of basalt and andesite that make excellent paleomagnetic recorders. Based on cross cutting relations and geochronologic data for pre-, syn-, and post-tectonic volcanic units, most of the faulting and tilting in the Sierra El Aguaje and Sierra Tinajas del Carmen is bracketed between 11.9 and 9.0 Ma, thus falling entirely within Proto-Gulf time. Existing field relations suggest the presence of large (>45°) vertical axis rotations in this region. This evidence includes: a) abrupt changes in the strike of tilted strata in different parts of the range b) ubiquitous NE-SW striking faults with left lateral-normal oblique slip, that terminate against major NW-trending right lateral faults, and c) obliquity between the general strike of tilted strata and the strike of faults. The results of the paleomagnetic investigation are consistent with the field evidence and show large clockwise rotations between ~30° and

  8. Deepwater Gulf of Mexico: high prospects

    International Nuclear Information System (INIS)

    The present and future role of the deepwater Gulf of Mexico to meeting natural gas requirements of the United States are reviewed.The steady increase in U.S. demand, outpacing U.S.supply for over 10 years and the increasing reliance by the USA on Canadian exports is demonstrated in conjunction with the '30 Tcf Challenge'. Regarding the Gulf of Mexico specifically, it is estimated that to meet expectations, production there needs to grow to 22 Bcfpd by 2020, especially the deepwater pools which have a potential of 80 to 140 Tcf over the next 50 years. These pools already produce as much oil as the shelf region, but only 25 per cent as much gas. To produce the expected 7 to 12 Bcfpd oil production must reach 4 million barrel of oil per day, which involves cycle time, new technologies and cost challenges. Much of the new technology needed is related to cutting costs and while good progress is being made, it is argued that further gains could occur if international technology were applied in the Gulf. The rate of success in exploration has also improved, with over one billion barrels of deepwater discoveries per year over the last four years. Cycle times have also improved, although the impact of cycle time in the deeper water regions is cause for some concern. The overall assessment is that to get the gas, one has to get the oil first, meaning that deepwater success is more dependent on oil prices than on gas prices. Nevertheless, the need for developing and applying new technologies remains paramount, including the application of existing foreign technologies that have proven successful elsewhere. It is equally important to demonstrate a high level of environmental stewardship, and to continue focusing on cycle time, including access to prospective acreage, a well-trained workforce, and reasonable regulatory and permitting requirements

  9. 76 FR 78245 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Gulf of Mexico Reef Fish Fishery...

    Science.gov (United States)

    2011-12-16

    ...NMFS, under the authority granted to the Secretary of Commerce (Secretary) under section 304(f) of the Magnuson-Stevens Fishery Conservation and Management Act (Magnuson-Stevens Act), has designated the South Atlantic Fishery Management Council (South Atlantic Council) as the responsible council to manage Nassau grouper in the Gulf of Mexico (Gulf) under the Fishery Management Plan (FMP) for......

  10. 75 FR 63786 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2010-10-18

    ... proposed temporary rule that would implement interim measures to reduce overfishing of gag in the Gulf of... this proposed rule is to reduce overfishing of the gag resource in the Gulf. DATES: Written comments... prevent overfishing and achieve, on a continuing basis, the optimum yield (OY) from Federally managed...

  11. Abundance and size of Gulf shrimp in Louisiana's coastal estuaries following the Deepwater Horizon oil spill.

    Directory of Open Access Journals (Sweden)

    Joris L van der Ham

    Full Text Available The Deepwater Horizon oil spill impacted Louisiana's coastal estuaries physically, chemically, and biologically. To better understand the ecological consequences of this oil spill on Louisiana estuaries, we compared the abundance and size of two Gulf shrimp species (Farfantepeneus aztecus and Litopeneus setiferus in heavily affected and relatively unaffected estuaries, before and after the oil spill. Two datasets were used to conduct this study: data on shrimp abundance and size before the spill were available from Louisiana Department of Wildlife and Fisheries (LDWF. Data on shrimp abundance and size from after the spill were independently collected by the authors and by LDWF. Using a Before-After-Control-Impact with Paired sampling (BACIP design with monthly samples of two selected basins, we found brown shrimp to become more abundant and the mean size of white shrimp to become smaller. Using a BACIP with data on successive shrimp year-classes of multiple basins, we found both species to become more abundant in basins that were affected by the spill, while mean shrimp size either not change after the spill, or increased in both affected and unaffected basins. We conclude that following the oil spill abundances of both species increased within affected estuaries, whereas mean size may have been unaffected. We propose two factors that may have caused these results: 1 exposure to polycyclic aromatic hydrocarbons (PAHs may have reduced the growth rate of shrimp, resulting in a delayed movement of shrimp to offshore habitats, and an increase of within-estuary shrimp abundance, and 2 fishing closures established immediately after the spill, may have resulted in decreased fishing effort and an increase in shrimp abundance. This study accentuates the complexities in determining ecological effects of oil spills, and the need of studies on the organismal level to reveal cause-and-effect relationships of such events.

  12. Spatial and temporal variability of freshwater discharge into the Gulf of Alaska

    Science.gov (United States)

    Hill, D. F.; Bruhis, N.; Calos, S. E.; Arendt, A.; Beamer, J.

    2015-02-01

    A study of the freshwater discharge into the Gulf of Alaska (GOA) has been carried out. Using available streamgage data, regression equations were developed for monthly flows. These equations express discharge as a function of basin physical characteristics such as area, mean elevation, and land cover, and of basin meteorological characteristics such as temperature, precipitation, and accumulated water year precipitation. To provide the necessary input meteorological data, temperature and precipitation data for a 40 year hind-cast period were developed on high-spatial-resolution grids using weather station data, PRISM climatologies, and statistical downscaling methods. Runoff predictions from the equations were found to agree well with observations. Once developed, the regression equations were applied to a network of delineated watersheds spanning the entire GOA drainage basin. The region was divided into a northern region, ranging from the Aleutian Chain to the Alaska/Canada border in the southeast panhandle, and a southern region, ranging from there to the Fraser River. The mean annual runoff volume into the northern GOA region was found to be 792 ± 120 km3 yr-1. A water balance using MODIS-based evapotranspiration rates yielded seasonal storage volumes that were consistent with GRACE satellite-based estimates. The GRACE data suggest that an additional 57 ± 11 km3 yr-1 be added to the runoff from the northern region, due to glacier volume loss (GVL) in recent years. This yields a total value of 849 ± 121 km3 yr-1. The ease of application of the derived regression equations provides an accessible tool for quantifying mean annual values, seasonal variation, and interannual variability of runoff in any ungaged basin of interest.

  13. Basin Hopping Graph

    DEFF Research Database (Denmark)

    Kucharik, Marcel; Hofacker, Ivo; Stadler, Peter;

    2014-01-01

    folding free energy landscape, however, can provide the relevant information. Results We introduce the basin hopping graph (BHG) as a novel coarse-grained model of folding landscapes. Each vertex of the BHG is a local minimum, which represents the corresponding basin in the landscape. Its edges connect...... basins when the direct transitions between them are “energetically favorable”. Edge weights endcode the corresponding saddle heights and thus measure the difficulties of these favorable transitions. BHGs can be approximated accurately and efficiently for RNA molecules well beyond the length range...

  14. Citizenship and migration in Arab Gulf monarchies

    DEFF Research Database (Denmark)

    Sater, J.

    2014-01-01

    , whereas fear and security concerns are often embedded in more populist debates. In the Arab Gulf region, as in many other regions, such as East Asia, this debate has taken distinctively different shapes, partially because the concept of citizenship remains a contested notion not just with regard to...... migrants, but also with regard to local populations. In addition to the contested nature of citizenship, migrants' lack of citizenship rights fulfils distinctive functions in what Saskia Sassen calls 'global cities'. This concept links the Arab world with a new phenomenon of globalized migration in which...

  15. 76 FR 21099 - Determinations Concerning Illnesses Discussed In National Academy of Sciences Reports on Gulf War...

    Science.gov (United States)

    2011-04-14

    ... Bromide, and Vaccines (66 FR 35702 (2001)); Gulf War and Health, Volume 2: Insecticides and Solvents (72 FR 48734 (2007)); Gulf War and Health: Updated Literature Review of Sarin (73 FR 42411 (2008)); Gulf War and Health, Volume 3: Fuels, Combustion Products, and Propellants (73 FR 50856 (2008)); Gulf...

  16. 78 FR 5403 - Fisheries of the Caribbean, Gulf, and South Atlantic; Aquaculture

    Science.gov (United States)

    2013-01-25

    ... the Fishery Management Plan for Regulating Offshore Marine Aquaculture in the ] Gulf of Mexico (FMP; formerly the Draft Generic Amendment to Gulf of Mexico Fishery Management Plans for Offshore Aquaculture... offshore aquaculture in Federal waters of the Gulf of Mexico (Gulf), other than live rock aquaculture...

  17. Early Mesozoic basin aquifers

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This data set represents the extent of the Early Mesozoic basin aquifers in the states of Massachusettes, Connecticut, New York, New Jersey, Pennsylvania, Maryland,...

  18. Mitigation : Closed Basin Project

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The upcoming meeting on waterfowl mitigation for the Closed Basin Project will have several people talk about possible changes to the waterfowl mitigation program....

  19. Tulare Basin protection plan

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — The Tulare Basin Protection Plan has been initiated by The Nature Conservancy to elucidate the problems and opportunities of natural diversity protection....

  20. California Air Basins

    Data.gov (United States)

    California Department of Resources — Air ResourcesCalifornia Air Resources BoardThe following datasets are from the California Air Resources Board: * arb_california_airbasins - California Air BasinsThe...

  1. K Basin Hazard Analysis

    International Nuclear Information System (INIS)

    This report describes the methodology used in conducting the K Basins Hazard Analysis, which provides the foundation for the K Basins Final Safety Analysis Report. This hazard analysis was performed in accordance with guidance provided by DOE-STD-3009-94, Preparation Guide for U. S. Department of Energy Nonreactor Nuclear Facility Safety Analysis Reports and implements the requirements of DOE Order 5480.23, Nuclear Safety Analysis Report

  2. K Basins Hazard Analysis

    International Nuclear Information System (INIS)

    This report describes the methodology used in conducting the K Basins Hazard Analysis, which provides the foundation for the K Basins Safety Analysis Report (HNF-SD-WM-SAR-062/Rev.4). This hazard analysis was performed in accordance with guidance provided by DOE-STD-3009-94, Preparation Guide for U. S. Department of Energy Nonreactor Nuclear Facility Safety Analysis Reports and implements the requirements of DOE Order 5480.23, Nuclear Safety Analysis Report

  3. The Ebro river basin

    OpenAIRE

    Darbra Roman, Rosa Maria

    2011-01-01

    River basins worldwide are under pressure from economic activities. In Europe, the two main factors hindering the achievement of good chemical and ecological status of European river basins are pollution, mainly coming from agriculture, and hydromorphology (e.g. for navigation, hydroelectricity and flood control). The economic activities affect the chemical and ecological status of rivers, lakes and groundwater and deplete available soil, sediments and water resources. The w...

  4. Offshore and onshore stratigraphic constraints to rebuild the evolution of the two conjugate margins (Gulf of Lion and West Sardinia) over the last 30 Myr

    Science.gov (United States)

    Leroux, Estelle; Gorini, Christian; Rubino, Jean-Loup; Rabineau, Marina; Aslanian, Daniel; Blanpied, Christian; Taillepierre, Rachel; Haq, Bilal

    2016-04-01

    Principles of seismic and sequential stratigraphy [Vail et al., 1977] are applied onto an extensive set of seismic reflection and drilling data in the Provençal Basin to correlate post-rift Miocene and Plio-Quaternary chronostratigraphic markers at the basin-wide scale. Stratigraphic, sedimentological and micropaleontological studies [Cravatte et al., 1974] for some of the boreholes provide additional information on the depositional environments and the chronostratigraphy of the drilled series. Synthesis of previous onshore studies on the both conjugate margins (Gulf of Lion and West Sardinia), and new fieldwork [Rueda, 2014] enable us to establish the stratigraphical link between onshore and offshore syn-rift and post-rift sequences. Miocene peri-Alpine foreland basin is particularly connected toward the south with the Gulf of Lion passive margin and is predominantly filled by marine shallow water siliciclastic deposits ranging from lower Miocene to Pliocene in age. Nine to ten depositional onshore sequences are identified [Besson et al., 2005, Rubino et al., 2015] and can be traced into the post rift part of the Gulf of Lion. The recognition of these sequences on the distal part of the shelf from the Burdigalian to the Messinian with a good well calibration is fully consistent and integrated in a chronostratigraphic history of the Provençal Basin over the last 30 Myr. We quantify, model and discuss the evolution of vertical movements and sediment budgets since the rifting. This study also allows us to construct a complete sea-level change curve for the western Mediterranean Neogene. Besson, D. (2005). Architecture du bassin rhodano-provençal miocène (Alpes, SE France). Relations entre déformation, physiographie et sédimentation dans un bassin molassique d'avant-pays (Doctoral dissertation, Paris, ENMP). Rueda, T. (2014). Analyse sédimentologique et stratigraphique du remplissage Oligo-Aquitanien du fossé du Campidano - Comparaison avec le remplissage

  5. Preliminary investigation of oil and source rock organic geochemistry from selected Tertiary basins of Thailand

    Science.gov (United States)

    Lawwongngam, Kulwadee; Philp, R. P.

    Selected samples of crude oils and extracts from source rocks obtained from six Thailand Tertiary basins of the central plain and of the Gulf of Thailand regions were examined for geochemical properties and molecular compositions. Analyses were performed using GC, CGCMS and carbon isotope mass spectrometry. Though these results should be viewed as preliminary, the results are significant in terms of a regional understanding of the petroleum geochemistry of Thailand. Results from bulk geochemical properties and biomarker assemblages characterize derivatives of organic sources deposited in lacustrine environments. The organic matter is mainly derived from algae with varying amounts of higher plant material. However, an observed variation in the pristane/phytane ratios among the samples may imply differences in depositional oxicity. On the other hand, basinal differences in sedimentation rates, or in the oxygen concentration of the varying waters and/or sediment pore-waters resulted in spatial heterogeneities in the quantity and degree of preservation of the organic matter. In addition, a degree of physical separation between these paleo-lacustrine environments is indicated by differences in paleosalinity, e.g. the hypersaline biomarker, gammacerane, which is restricted to samples from the offshore Gulf of Thailand basins. Maturity parameters for these Tertiary oils and source rock extracts were determined using biomarker analyses of T s/T m, 22S/22S + 22R C 31 hopane, C 30 moretane/hopane, 20R/20S + 20R C 29 sterane, and aromatic compounds. Though the samples demonstrate an overall relatively low level of maturity as specified by the biomarker index, a degree of individual basinal variability is also distinguishable. The observed differences in the maturity values indicate regional heterogeneity among the basin thermal histories, suggesting differences in geothermal gradients and/or in the basin subsidence rates.

  6. Plate boundary deformation at the latitude of the Salton Trough - northern Gulf of California (Invited)

    Science.gov (United States)

    Stock, J. M.

    2013-12-01

    Along the Pacific-North America plate boundary zone, the segment including the southern San Andreas fault to Salton Trough and northern Gulf of California basins has been transtensional throughout its evolution, based on Pacific-North America displacement vectors calculated from the global plate circuit (900 × 20 km at N54°W since 20 Ma; 460 × 20 km at N48°W since 11 Ma). Nevertheless, active seismicity and focal mechanisms show a broad zone of plate boundary deformation within which the inferred stress regime varies locally (Yang & Hauksson 2013 GJI), and fault patterns in some regions suggest ongoing tectonic rotation. Similar behavior is inferred to have occurred in this zone over most of its history. Crustal structure in this region is constrained by surface geology, geophysical experiments (e.g., the 2011 Salton Seismic Imaging Project (SSIP), USGS Imperial Valley 1979, PACE), and interdisciplinary marine and onland studies in Mexico (e.g., NARS-Baja, Cortes, and surveys by PEMEX). Magnetic data (e.g., EMAG-2) aids in the recognition of large-scale crustal provinces and fault boundaries in regions lacking detailed geophysical surveys. Consideration of existing constraints on crustal thickness and architecture, and fault and basin evolution suggests that to reconcile geological deformation with plate motion history, the following additional factors need to be taken into account. 1) Plate boundary displacement via interacting systems of rotating blocks, coeval with slip on steep strike slip faults, and possibly related to slip on low angle extensional faults (e.g, Axen & Fletcher 1998 IGR) may be typical prior to the onset of seafloor spreading. This fault style may have accommodated up to 150 km of plate motion in the Mexican Continental Borderland and north of the Vizcaino Peninsula, likely between 12 and 15 Ma, as well as explaining younger rotations adjacent to the Gulf of California and current deformation southwest of the Salton Sea. 2) Geophysical

  7. Numerical model of circulation and residence times in the Persian Gulf

    Science.gov (United States)

    O'Donncha, Fearghal; Ragnoli, Emanuele

    2014-05-01

    The Persian Gulf is a semi-enclosed, marginal sea that is exposed to arid, subtropical climate. As a consequence of the extreme climate, evaporation is greater than freshwater inflow resulting in a net loss of water and associated, reverse flow, estuarine circulation as the highly saline waters exit the basin through the Straits of Hormuz, into the Gulf of Oman. Because of their consistent direction, these density currents are central in the distribution and removal of pollutants from the gulf. Tidal forcing impacts circulation in the region, particularly on smaller scales of length and time. Wind forcing can be significant, particularly the Shamal weather phenomenon; wind that sets in with great abruptness and force, and is related to synoptic weather systems to the Northwest. Output from high resolution (~1km) numerical simulations, using NEMO (Nucleus for European Modelling of the Ocean), provide insight into the physical oceanography of the region. The model was forced by 0.75° European Centre for Medium-Range Weather Forecasts (ECMWF) atmospheric data and tidal constituents extracted from the Oregon State University Tidal Prediction Software (OTPS/TPXO). Model results permit a detailed examination of the three primary forcing processes, namely: tidal forces, wind forces, and density differences. To assess fundamental model performance, results are compared with two historical observation datasets: (1) a comprehensive dataset of velocity and CTD measurements collected by Reynolds (1993) and (2) time series measurements recorded in the Strait of Hormuz from December 1996 to March 1998 by Johns et al. (2003). Model results exhibit close agreement to field values validating the model for a more detailed analysis of circulations patterns within the gulf. To better elucidate the dominant forcing processes, classical tidal analysis decomposed the flow currents by fitting the flow profile to a finite set of sinusoids at specific frequencies related to astronomical

  8. Report A, chemical oceanographic data from the Persian Gulf and Gulf of Oman from 17 April 1972 to 17 March 1978 (NODC Accession 7900091)

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Temperature profile and chemical data were collected using bottle casts from NOAA Ship DELAWARE and other platforms in the Persian Gulf and Gulf of Oman from 17...

  9. Northern Gulf Littoral Initiative (NGLI), Geology and Physical Properties of Marine Sediments in the N.E. Gulf of Mexico: Data Report

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — The Northern Gulf Littoral Initiative (NGLI), Geology and Physical Properties of Marine Sediments in the N.E. gulf of Mexico: Data Report, was produced by the U.S....

  10. Population Structure, Abundance and Movement of Whale Sharks in the Arabian Gulf and the Gulf of Oman

    Science.gov (United States)

    Robinson, David P.; Jaidah, Mohammed Y.; Bach, Steffen; Lee, Katie; Jabado, Rima W.; Rohner, Christoph A.; March, Abi; Caprodossi, Simone; Henderson, Aaron C.; Mair, James M.; Ormond, Rupert; Pierce, Simon J.

    2016-01-01

    Data on the occurrence of whale sharks, Rhincodon typus, in the Arabian Gulf and Gulf of Oman were collected by dedicated boat surveys and via a public-sightings scheme during the period from 2011 to 2014. A total of 422 individual whale sharks were photo-identified from the Arabian Gulf and the northern Gulf of Oman during that period. The majority of sharks (81%, n = 341) were encountered at the Al Shaheen area of Qatar, 90 km off the coast, with the Musandam region of Oman a secondary area of interest. At Al Shaheen, there were significantly more male sharks (n = 171) than females (n = 78; X2 = 17.52, P 9 m individuals were visually assessed as pregnant. Connectivity among sharks sighted in Qatari, Omani and UAE waters was confirmed by individual spot pattern matches. A total of 13 identified sharks were re-sighted at locations other than that at which they were first sighted, including movements into and out of the Arabian Gulf through the Strait of Hormuz. Maximum likelihood techniques were used to model an estimated combined population for the Arabian Gulf and Gulf of Oman of 2837 sharks ± 1243.91 S.E. (95% C.I. 1720–6295). The Al Shaheen aggregation is thus the first site described as being dominated by mature males while the free-swimming pregnant females are the first reported from the Indian Ocean. PMID:27362839

  11. The origin of islands in the Kandalaksha Gulf of the White Sea: joint work of internal and external geodynamic processes

    Science.gov (United States)

    Kosevich, Natalia; Romanovskaya, Maria

    2016-04-01

    The modern White Sea basin is a part of the encounter zone between the East European Platform and of the Fennoscandian Shield. The Kandalaksha Gulf in its northwest lies on the Mesoarchean-Paleoproterozoic structure known as the White Sea Shift Belt. In the Oligocene, it entered its neotectonic stage. Geologically, there are two structural storeys beneath the seafloor of the Kandalaksha Gulf: 1) crystalline bedrock of the Archean White Sea complex; 2) a cover of sediment consisting of three layers: Riphean sandstones, terrigenous Vendian deposits; a cloak of Pleistocene and Holocene deposits and sediments - glacial drifts, transitional glaciomarine sediments and purely marine sediments. The modern White Sea is a young basin formed just 10 to 12 ka. The geological and geomorphic history of the White Sea region was very complicated, with various and often conflicting tectonic movements. Besides the postglacial isostatic rise of Scandinavia amounted to some 100 meters in the White Sea area. The White Sea has numerous islands that are very different in the geological-geomorphological and genetic senses because their origin is the result of interactions between various endogenous and exogenous processes. Large and detailed scale geological and morphological researches of the islands at the southern and northern coast of the Kandalaksha Gulf have been carried out. Landforms of the islands were produced by the joint effects of such processes as (1) glacial-tectonic effects and marine wave action, (2) tidal and surge effects; (3) glacial-tectonic, marine, and gravity effects, and (4) glacial-tectonic, marine, lake, and biogenic effects (Kosevich, 2015). The relief structure of the islands has the following regularities: 1) structures of the northern coast islands are more often landforms that are composed of loose deposits with small sites of structural denudation residual outcrops; 2) the structures of the southern coast islands are typically combinations of loose

  12. Mesoscale eddies in the Gulf of Aden and their impact on the spreading of Red Sea Outflow Water

    Science.gov (United States)

    Bower, Amy S.; Furey, Heather H.

    2012-04-01

    The Gulf of Aden (GOA) in the northwestern Indian Ocean is the receiving basin for Red Sea Outflow Water (RSOW), one of the World’s few high-salinity dense overflows, but relatively little is known about spreading pathways and transformation of RSOW through the gulf. Here we combine historical data, satellite altimetry, new synoptic hydrographic surveys and the first in situ direct observations of subsurface currents in the GOA to identify the most important processes in the spreading of RSOW. The new in situ data sets were collected in 2001-2003 as part of the Red Sea Outflow Experiment (REDSOX) and consist of two CTD/LADCP Surveys and 49 one-year trajectories from acoustically tracked floats released at the depth of RSOW. The results indicate that the prominent positive and negative sea level anomalies frequently observed in the GOA with satellite altimetry are associated with anticyclonic and cyclonic eddies that often reach to at least 1000 m depth, i.e., through the depth range of equilibrated RSOW. The eddies dominate RSOW spreading pathways and help to rapidly mix the outflow water with the background. Eddies in the central and eastern gulf are basin-scale (∼250-km diameter) and have maximum azimuthal speeds of about 30 cm/s at the RSOW level. In the western gulf, smaller eddies not detectable with satellite altimetry appear to form as the larger westward-propagating eddies impale themselves on the high ridges flanking the Tadjura Rift. Both the hydrographic and Lagrangian observations show that eddies originating outside the gulf often transport a core of much cooler, fresher water from the Arabian Sea all the way to the western end of the GOA, where the highest-salinity outflow water is found. This generates large vertical and horizontal gradients of temperature and salinity, setting up favorable conditions for salt fingering and diffusive convection. Both of these mixing processes were observed to be active in the gulf. Two new annually appearing

  13. Obesity, diabetes and longevity in the Gulf: is there a Gulf Metabolic Syndrome?

    OpenAIRE

    Guy, Geoffrey W.; Nunn, Alistair V.W.; Thomas, Louise E; Bell, Jimmy D.

    2009-01-01

    The Gulf is experiencing a pandemic of lifestyle-induced obesity and type 2 diabetes mellitus (T2DM), with rates exceeding 50 and 30%, respectively. It is likely that T2DM represents the tip of a very large metabolic syndrome iceberg, which precedes T2DM by many years and is associated with abnormal/ectopic fat distribution, pathological systemic oxidative stress and inflammation. However, the definitions are still evolving with the role of different fat depots being critical. Hormetic stimul...

  14. Diphytanyl glycerol ether distributions in sediments of the Orca Basin

    Science.gov (United States)

    Pease, Tamara K.; Van Vleet, Edward S.; Barre, Jill S.

    1992-09-01

    Archaebacterially produced diphytanyl glycerol ether (DPGE) was examined in core sediments from the Orca Basin, an anoxic hypersaline basin in the northwestern Gulf of Mexico, to observe its spatial variability and potential origin. A differential extraction protocol was employed to quantify the isopranyl glycerol ethers associated with unbound, intermediate-bound, and kerogen-bound lipid fractions. Archaebacterial lipids were evident at all depths for the unbound and intermediate-bound fractions. Concentrations of DPGE ranged from 0.51 to 2.91 μg/g dry sediment at the surface and showed secondary maxima deeper in basin sediments. Intermediate-bound DPGE concentrations exhibited an inverse relationship to unbound DPGE concentrations. Kerogen-bound DPGE concentrations were normally below detection limits. Earlier studies describing the general homogeneity of lipid components within the overlying brine and at the brine/seawater interface suggest that the large-scale sedimentary DPGE variations observed in this study result from spatial and temporal variations in in situ production by methanogenic or extremely halophilic archaebacteria.

  15. Pliocene-Quaternary contourites along the northern Gulf of Cadiz margin: sedimentary stacking pattern and regional distribution

    Science.gov (United States)

    Llave, Estefanía; Matias, Hugo; Hernández-Molina, F. Javier; Ercilla, Gemma; Stow, Dorrik A. V.; Medialdea, Teresa

    2011-12-01

    This study reports novel findings on the Pliocene-Quaternary history of the northern Gulf of Cadiz margin and the spatiotemporal evolution of the associated contourite depositional system. Four major seismic units (P1, P2, QI and QII) were identified in the Pliocene-Quaternary sedimentary record based on multichannel seismic profiles. These are bounded by five major discontinuities which, from older to younger, are the M (Messinian), LPR (lower Pliocene revolution), BQD (base Quaternary discontinuity), MPR (mid-Pleistocene revolution) and the actual seafloor. Unit P1 represents pre-contourite hemipelagic/pelagic deposition along the northern Gulf of Cadiz margin. Unit P2 reflects a significant change in margin sedimentation when contourite deposition started after the Early Pliocene. Mounded elongated and separated drifts were generated during unit QI deposition, accompanied by a general upslope progradation of drifts and the migration of main depocentres towards the north and northwest during both the Pliocene and Quaternary. This progradation became particularly marked during QII deposition after the mid-Pleistocene (MPR). Based on the spatial distribution of the main contourite depocentres and their thickness, three structural zones have been identified: (1) an eastern zone, where NE-SW diapiric ridges have controlled the development of two internal sedimentary basins; (2) a central zone, which shows important direct control by the Guadalquivir Bank in the south and an E-W Miocene palaeorelief structure in the north, both of which have significantly conditioned the basin-infill geometry; and (3) a western zone, affected in the north by the Miocene palaeorelief which favours deposition in the southern part of the basin. Pliocene tectonic activity has been an important factor in controlling slope morphology and, hence, influencing Mediterranean Outflow Water pathways. Since the mid-Pleistocene (MPR), the sedimentary stacking pattern of contourite drifts has been

  16. 78 FR 66945 - Proposed Collection; 60-Day Comment request: Gulf Long-Term Follow-Up Study (GuLF STUDY)

    Science.gov (United States)

    2013-11-07

    ... Follow-Up Study (GuLF STUDY) Summary: In compliance with the requirement of Section 3506(c)(2)(A) of the... Follow-Up Study (GuLF STUDY), 0925-0626, Expiration Date 01/31/2014--REVISION, National Institute of... Collection: The purpose of the GuLF STUDY is to investigate potential short- and long-term health...

  17. Screening specifications for Gulf Coast salt domes

    International Nuclear Information System (INIS)

    A reconnaissance survey of the salt domes of Mississippi, Louisiana, and east Texas is being planned to identify study areas for potential sites for radioactive waste disposal. Preliminary screening specifications were derived for each of the geological evaluation criteria by application of the significant factors that will have an impact on the reconnaissance survey. The procedure for the derivation of each screening specification is discussed. The screening specifications are the official OWI values to be used for the first-cut acceptance for salt dome study areas along the Gulf Coast. The derivation of the screening specifications is illustrated by (1) a statement of the geological evaluation criterion, (2) a discussion of the pertinent factors affecting the criterion, and (3) the evaluation of the value of the specification

  18. New era in Gulf of Mexico seismic

    Energy Technology Data Exchange (ETDEWEB)

    Hamilton, H.; Brune, R. [TGS-Calibre Geophysical Co., Houston, TX (United States)

    1996-05-01

    The 1990s have seen tremendous changes in seismic activity in the Gulf of Mexico (GOM). Until the 1980s, seismic surveys in the GOM, particularly 3-D, were almost always proprietary. From 1990 to 1993, activity shifted so that now nearly all seismic surveys are non-exclusive 3-D, available for license by any operator. An obvious motivation for this shift was the reduced costs to E and P companies. Technical reasons also motivated this shift. Larger surveys have halos sufficient to image steeper dips and deeper targets, and allow analysis of complex regional geologic settings. This paper briefly summarizes the new technologies, trends in 3-D usage, ocean bottom cabling, data processing, data quality, and navigational tracking systems.

  19. Northern Gulf of Mexico Marine Mammal Unusual Mortality Event Database

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Tissues and samples collected from marine mammals during investigation of the Northern Gulf of Mexico Marine Mammal Unusual Mortality Event are tracked within this...

  20. GAOCMAO and its oil spill response activities in the Gulf

    International Nuclear Information System (INIS)

    Gulf Area Oil Companies Mutual Aid Organisation (GAOCMAO), has taken active steps in cooperation with its member companies, national and regional environmental organisation (ROPME) in an attempt to protect the Gulf from various sources of pollution. Specific attention was given to oil pollution response in terms of stockpiling of adequate equipment, training of personal and coordination through the application of pre-prepared contingency plans. All these activities tell us that a lot has been done to protect the Gulf environment from pollution. GAOCMAO, after many years of successful development looks to the future with confidence and renewed vigor. It is the intention of this organisation to enhance its member companies capabilities to respond to major incidents and to work closely with the national governmental, regional and international environmental organisations throughout the world, in fields appropriate to the Gulf oil industry. (author)

  1. Gulf of Maine Contaminated Sediments Database (GOMCSDB shapefile)

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — The Contaminated Sediments Database for the Gulf of Maine provides a compilation and synthesis of existing data to help establish the environmental status of our...

  2. Water Stratification Raster Images for the Gulf of Maine

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This geodatabase contains seasonal water stratification raster images for the Gulf of Maine. They were created by interpolating water density (sigma t) values at 0...

  3. Gulf of Mexico killer whale photo-ID catalog

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Photo-identification data on killer whales occupying the northern Gulf of Mexico have been collected in association with large vessel surveys since 1991....

  4. Future role of Gulf oil in world energy demand

    International Nuclear Information System (INIS)

    The view that there will be a growing dependence on oil from the Gulf countries is shared by a great number of oil market analysts. This view is based on the fact that Gulf countries dominate the global oil reserves. Energy analyst argue that as the world demand for oil continues to grow driven largely by the growth in developing countries' consumption coupled with constrained non-OPEC supply, the end result will be that the call on Gulf oil will grow substantially. In summary, this paper has challenged the view of growing dependence on oil from the Gulf using available information in conjunction with reasonable and fairly plausible arguments. The aim was to point out to the GCC member counties the danger of relying on these views in shaping their economic policies and in setting their oil market strategies. They may run the ultimate risk of being left with huge oil reserves that no one wants. (orig.)

  5. 2009 Survey of Gulf of Mexico Dockside Seafood Processors

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This survey gathered and analyze economic data from seafood processors throughout the states in the Gulf region. The survey sought to collect financial variables...

  6. Gulf sturgeon Critical Habitat Units 1-7

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — These data represent the critical habitat for Gulf Sturgeon as designated by Federal Register Vol. 68, No. 53, Wednesday, March 19, 2003, Rules and Regulations.

  7. 2012 Economic Survey of Gulf State Shrimp License Holders

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This mail survey collected economic data on inshore commercial shrimp fishermen who held licenses to commercially harvest shrimp in state waters of the U.S. Gulf of...

  8. Gulf of Mexico Kemps ridley sea turtle age and growth

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This study involves analysis of skeletal growth marks in humerus bones of 340 Kemps ridley sea turtles stranded dead along the Gulf of Mexico US coast (hatchling to...

  9. EAARL Topography-Gulf Islands National Seashore-Florida

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Elevation maps (also known as Digital Elevation Models or DEMs) of Gulf Islands National Seashore were produced from remotely-sensed, geographically-referenced...

  10. Shipping Fairways in the Gulf of Mexico, from BOEM

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Polygon data for all major shipping lanes associated with all ports in the Gulf of Mexico are presented. These layers were modified from GIS data acquired from the...

  11. EAARL Topography-Gulf Islands National Seashore-Mississippi

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Abstract: Elevation maps (also known as Digital Elevation Models or DEMs) of Gulf Islands National Seashore were produced from remotely-sensed,...

  12. Gulf of Mexico Protected Species Assessment Aerial Surveys

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — These data sets include a compilation of aerial line-transect surveys conducted over continental shelf waters of the Gulf of Mexico since 1992. The majority of...

  13. EAARL Coastal Topography - Northern Gulf of Mexico, 2007: Bare earth

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — A bare earth elevation map (also known as a Digital Elevation Model, or DEM) of the northern Gulf of Mexico barrier islands and Naval Live Oaks was produced from...

  14. Gulf of Maine Cooperative Bottom Longline Survey Database

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This database is for a bottom longline (fixed gear) survey executed in the western and central Gulf of Maine targeting complex rocky habitats. The survey is...

  15. Gulf of Mexico Marine Mammal Assessment Vessel Surveys

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — These data sets are a compilation of large vessel surveys for marine mammal stock assessments in the Gulf of Mexico from 1991 to the present. These are designed as...

  16. EAARL Coastal Topography - Northern Gulf of Mexico, 2007: First surface

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — A first surface elevation map (also known as a Digital Elevation Model, or DEM) of the northern Gulf of Mexico barrier islands and Naval Live Oaks was produced from...

  17. Gulf of Mexico sperm whale photo-ID catalog

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Photo-identification data on sperm whales occupying the north central Gulf of Mexico have been collected during vessel surveys. Photographs of sperm whales are...

  18. Gulf of Mexico Sperm Whale Acoustic Prey Study

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Large vessel surveys were conducted during the summer of 2009 and the winter of 2010 in the north-central Gulf of Mexico to examine the spatial distribution of...

  19. Biogeography of Nearshore Subtidal Invertebrates in the Gulf of Maine

    Science.gov (United States)

    The biogeography of nearshore benthic invertebrates in the Gulf of Maine was studied to compare recent data with historical biogeographic studies, define physical-chemical factors affecting species distributions, and provide information needed to calibrate benthic indices of envi...

  20. Mercury levels in seabirds in the Gulf of Maine

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — We conducted a pilot study to screen mercury Hg levels in Gulf of Maine seabirds in an effort to determine which species are most at risk, are the most appropriate...

  1. Gulf sturgeon Critical Habitat Units 8-14

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — These data represent the critical habitat for Gulf Sturgeon as designated by Federal Register Vol. 68, No. 53, Wednesday, March 19, 2003, Rules and Regulations.

  2. Directional wave measurements off Navinal, Gulf of Kachchh, India

    Digital Repository Service at National Institute of Oceanography (India)

    Vethamony, P.; KrishnaKumar, V.; Suryanarayana, A.; Antony, M.K.; Swamy, G.N.

    Results of directional wave measurements carried out off Navinal, Gulf of Kachchh representing pre-monsoon and southwest monsoon wave conditions are presented. Maximum wave height encountered during pre-monsoon and southwest monsoon is 1.36 and 1...

  3. The Neolithic origins of seafaring in the Arabian Gulf

    Directory of Open Access Journals (Sweden)

    Robert Carter

    2002-10-01

    Full Text Available The inhabitants of the Arabian Gulf were among the world’s earliest maritime traders. Their ships sailed regularly between the Bronze Age civilizations of Mesopotamia, Bahrain and the Indus Valley, and they reached China by sea in the eighth century AD, thus bypassing the long and perilous overland Silk Road route across Central Asia. Now excavations at a coastal site in Kuwait by a team from the Institute have revealed even earlier evidence of maritime activity in the Gulf.

  4. Carnosine Treatment for Gulf War Illness: A Randomized Controlled Trial

    OpenAIRE

    Baraniuk, James Nicholas; El-Amin, Suliman; Corey, Rebecca; Rayhan, Rakib; Timbol, Christian

    2013-01-01

    About 25% of 1990-1991 Persian Gulf War veterans experience disabling fatigue, widespread pain, and cognitive dysfunction termed Gulf War illness (GWI) or Chronic Multisymptom Illness (CMI). A leading theory proposes that wartime exposures initiated prolonged production of reactive oxygen species (ROS) and central nervous system injury. The endogenous antioxidant L-carnosine (β-alanyl-L-histidine) is a potential treatment since it is a free radical scavenger in nervous tissue. To determine if...

  5. Sperm whales (Physeter catodon) in the Gulf of Mexico

    Science.gov (United States)

    Collum, L.A.; Fritts, T.H.

    1985-01-01

    The distribution of the sperm whale, Physeter catodon, was documented in the Gulf of Mexico during 1979 to 1981 using regular aerial surveys and opportunistic sightings from ships. Most sightings were in the western Gulf of Mexico in deep waters near the edge of the continental shelf. A total of 47 adults and 12 young animals was sighted in groups containing from one to 14 animals.

  6. WiBasin: basin management through an integrated platform

    OpenAIRE

    Llort Pavon, Xavier; Sánchez-Diezma Guijarro, Rafael; Sancho, David; Rodríguez, Álvaro; Berenguer Ferrer, Marc; Sempere Torres, Daniel

    2014-01-01

    In this work we present WiBasin, a cloud platform for basin and dam management. It includes different sources of precipitation (both observed and forecasted), integration over the catchment domain (to provide an aggregated value of potential rainfall accumulated over the basin) , and a complete dissemination environment (web-viewer, capability of issuing hazard warnings with configurable thresholds, SMS, mails, etc.)

  7. Evolution and timing of salt diapirism in the Iranian sector of the Persian Gulf

    Science.gov (United States)

    Perotti, Cesare; Chiariotti, Luca; Bresciani, Ilenia; Cattaneo, Luciano; Toscani, Giovanni

    2016-06-01

    The Iranian sector of the Persian Gulf is affected by more than 30 large diapiric structures triggered by the mobilization of the Infracambrian Hormuz Complex, an evaporite-rich unit that overlies Precambrian basement at the base of the sedimentary succession. Nineteen non-piercing diapirs, without any appreciable salt intrusion into the upper succession, were studied in detail and retro-deformed by the decompaction and unfolding of 13 seismic horizons that were identified by the interpretation of a dense grid of 2D seismic lines and calibrated by well data. Salt uplift had begun by the Early Palaeozoic and persists to the present day, with major pulses of intensity during the Middle Triassic, Cenomanian, Late Oligocene, and post-Middle Miocene. The structural reconstructions and the analysis of the progressive deformation of the study diapirs do not show any link between diapiric uplift and local tectonic structures, and no clear correlation with the regional geodynamic events acting at the boundary of the Arabian plate. On the contrary, the salt uplift seems strongly influenced by the differential rate of sedimentation that affected the whole study basin (more than 40,000 km2), with a coefficient of correlation between the salt uplift rate and the differential rate of sedimentation (expressed by the standard deviation of the sedimentation rate calculated over the entire basin) of 0.95. This downbuilding mechanism of diapiric growth is apparently induced by differential sedimentation over long distances (several tens of kilometers), showing that the flow of salt affected the whole basin and not just the areas around the single diapiric structures.

  8. Voluntary Challenge and Registry action plan: Gulf Canada Resources Limited

    International Nuclear Information System (INIS)

    The overall paper deals with: a company overview, Gulf's approach to the Action Plan, emissions inventory and indices, goals and objectives, progress report on actions, emission projection, domestic offsets and joint implementation, and summary. Gulf Canada Resources Ltd. is a publicly traded, Canadian oil and gas company that explores, produces and markets conventional, heavy and synthetic crude oil, natural gas liquids, natural gas and sulfur around the world. Gulf's Action Plan goal is to attain GHG emissions at or below 1990 levels. By maintaining a record of actions taken and the results produced, Gulf will better be able to adapt to more stringent protocols that may be adopted post-Kyoto. Gulf's goals are: to maintain or reduce emission rates per unit of energy equivalent production over the long term, focus on GHG reduction actions and measures that meet the company's economic objectives, and remain abreast of current and projected directions of international emissions protocol. A status report is included on the actions that have been completed since the last report and those that are planned. Completed or planned actions are summarized on: energy efficiency, gas capture, acid gas injection, and others. Observations and conclusions are offered by Gulf regarding their inventory and analysis. 1 tab

  9. Oil spill in the Gulf of Mexico and spiral vortex

    Institute of Scientific and Technical Information of China (English)

    ZHENG Quanan; ZHAO Qing; Nan Walker; LI Chunyan

    2010-01-01

    @@ Drilling rig Decpwater Horizon in the Gulf of Mexico, leased by BP PLC from Transocean Ltd., ex-ploded and caught on fire on April 20, 2010. The drilling location is at some 50 miles (80 kilometers) off the coast of Louisiana, USA. The rig sank on April 22. Since then, oil has been pouring into the Gulf from the blown-out undersea well. As reported by US Today and Calgary Herald on July 3, an estimated 35 000 to 60 000 barrels of oil per day has been gush-ing out of the ruptured well into the Gulf. That means amounts to a total of 1.9 to 3.6 million barrels of oil so far have gushed into the Gulf. Using the high end of that estimate, the spill has now surpassed the 1979 Ixtoc blowout, which took nine months to cap and dumped estimated 3.3 million barrels (140 000 million gallons) into the Gulf of Mexico. It is topped only by the deliberate release of six to eight million barrels of crude oil by Iraqi troops who destroyed tankers and oil terminals and set wells ablaze in Kuwait during the 1991 Gulf War.

  10. Grain size distribution, clay mineralogy and chemistry of bottom sediments from the outer Thermaikos Gulf, Aegean Sea, Greece

    Directory of Open Access Journals (Sweden)

    K.G. PEHLIVANOGLOU

    2012-12-01

    Full Text Available The Thermaikos Gulf constitutes the NW part of the North Aegean Sea and is limited eastward from the Chalkidiki Peninsula and westward from the Pieria Prefecture. Its plateau covers an area of 3,500 km2. The mechanisms responsible for the grain size distribution into the Gulf, the clay mineralogy and the chemistry of some bottom sediments from the outer Thermaikos Gulf, are examined. Source mixing during transportation, flocculation, differential settling processes and organic matter appear to be the main mechanisms for the distribution of clay minerals in shallow waters. All grain size fractions studied present a wide range of values confirming the extreme variations of the discharged load and the variability in marine processes. Plagioclases predominate over K-feldspars, while quartz is the most abundant mineral present. In addition, micas, chlorites, amphiboles and pyroxenes exist as primary and/or accessory minerals in all samples. Among clay minerals, illite predominates over smectite and smectite over chlorite (+ kaolinite. The ordered interstratified phase of I/S, with 30-35% S layers, is present in the 2-0.25µm fraction. The randomly interstratified phase of I/S, with 50% S layers, is present in the <0.25& micro; m fraction. On average the clay mineral content of the studied samples is: 48% I, 23% S, 17% Ch (+K and 12% others for the 2-0.25µm fraction and 50% I, 30% S and 20% Ch (+K for the <0.25 µm fraction. All these minerals are the weathering products of the rocks from the drainage basins of the rivers flowing into the Gulf, as well as of the Neogene and Quaternary unconsolidated sediments of the surrounding coasts. The terrigenous input, the water mass circulation and, to a lesser extent, the quality of the discharged material and the differential settling of grains, control the grain size distribution within the outer Thermaikos Gulf. The chemical composition of the analysed samples is generally in agreement with their mineral

  11. Isotopic characterization and genetic origin of crude oils from Gulf of Suez and western desert fields in Egypt

    International Nuclear Information System (INIS)

    Stable carbon isotopes were used to asses the general characteristics of the western desert and Gulf of Suez crude oils in accordance with hydrocarbon generation, source rocks, thermal gradient and maturation level. The carbon isotopic results of all the analyzed oil samples in both areas lie in the range from -29.62 to -24.11 %. The av. σ 13C values in the Gulf of Suez reaches about -28.6% and -26.4% in western desert. It was accounted a marginal difference between the two areas by about 2.5 : 3% in carbon-13 isotope of the whole oil indicated two distinct oil types of different organic input and varies in the depositional environment. It was found that Gulf of Suez oils are dominated by marine organic matter (plankton algae) deposited in saline environment. The derived oils from the northern and central provinces of the Gulf are isotopically light, higher in sulfur content, lower in API gravity degree and have Pristane/Phytane (Pr/Ph) ratio less than or equal one (Pr/Ph = 1). In the southern province, about 0.5% isotopic enrichment was recorded in the produced oils from shallower depths, associated with gradual increment in API and maturity level as thermal gradient increase. However, low API gravity degree and less maturity of the Gulf of Suez oils could be related to the rifting temperature that forced and accelerated the expulsion rate and hydrocarbon generation prior reaching higher maturation levels. On the other hand, the produced oils from the western desert fields belong mostly to terrestrial organic debris (with minor marine fragment in some basins) deposited at deeper geological formations. It is characterized by isotopic enrichment, paraffinic waxy oils, low in sulphur content, have Pr/Ph = 1, high in API gravity and maturity level. Hydrocarbon generated from the western desert fields has been controlled by time-temperature effect in the source rocks and reservoirs where the humic organic matter are affected by high temperature over longer period of

  12. Modifed Great Basin Extent (Buffered)

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — Two different great basin perimeter files were intersected and dissolved using ArcGIS 10.2.2 to create the outer perimeter of the great basin for use modeling...

  13. Anthropogenic and authigenic uranium in marine sediments of the central Gulf of California adjacent to the Santa Rosalía mining region

    OpenAIRE

    Shumilin, Evgueni; Rodríguez Figueroa, Griselda Margarita; Sapozhnikov, Dmitry; Sapozhnikov, Yuri; Choumiline, Konstantin

    2012-01-01

    To investigate the causes of uranium (U) enrichment in marine sediments in the eastern sector of the Gulf of California, surface sediments and sediment cores were collected adjacent to the Santa Rosalı´a copper mining region in the Baja California peninsula. Three coastal sediment cores were found to display high concentrations of U (from 54.2 ± 7.3 mg kg-1 to 110 ± 13 mg kg-1) exceeding those found in the deeper cores (1.36 ± 0.26 mg kg-1 in the Guaymas Basin to 9.31 ± 3.03 mg kg-1 in the SR...

  14. 76 FR 43250 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Stone Crab Fishery of the Gulf of...

    Science.gov (United States)

    2011-07-20

    ... action is to enhance the effectiveness and efficiency of managing the stone crab fishery in the Gulf of... Microsoft Word, Excel, WordPerfect, or Adobe PDF file formats only. Comments received through means...

  15. Geology Arc Export Layer From Coal Bearing Geology of the Gulf Coast Coal Region (gulf_geol_dd.e00)

    Data.gov (United States)

    U.S. Geological Survey, Department of the Interior — This dataset is a polygon vector coverage of coal bearing geologic units that occur in states which comprise the Gulf Coast Coal Assessment Region as defined by the...

  16. Reversing the indus basin closure

    OpenAIRE

    2011-01-01

    After independence, a swift and extensive development of Indus river basin has intensified commitment of water resources. During dry period, the indication of over commitment and basin closure are visible. In the beginning 2000s, he river basin water resources were committed to more than 99% without any environmental flows. The paper tries to unfold drivers closing the Indus basin and the scope for change. Defining and implementing water allocation mechanism to ascertain equity, sustainabilit...

  17. Final report on Paradox Basin/Gulf Interior: Regulatory project management

    International Nuclear Information System (INIS)

    This final report on the Regulatory Project Manager (RPM) program begins with a discussion of the key products produced during the 9-year effort and then focuses on the work performed in the major disciplines. The report then discusses the management of the work effort and the Quality Assurance (QA) program. It concludes with a brief discussion of the records turned over to the Office of Nuclear Waste Isolation (ONWI) at the conclusion of the work. 14 figs., 14 tabs

  18. South Bohemian basins

    Czech Academy of Sciences Publication Activity Database

    Spudil, J.; Brož, B.; Dašková, Jiřina; Holcová, K.; Kvaček, Z.; Pešek, J.; Svobodová, Marcela; Sýkorová, Ivana; Teodoridis, V.

    Prague: Czech Geological Survey, 2014, s. 190-206 ISBN 978-80-7075-862-5 R&D Projects: GA ČR GA105/06/0653 Institutional support: RVO:67985891 ; RVO:67985831 Keywords : Tertiary basins * Czech Republic * Cenomanian and Tertiary lignite * geology * stratigraphy Subject RIV: DB - Geology ; Mineralogy

  19. Pasco Basin hydrometeorological study

    International Nuclear Information System (INIS)

    This report provides detailed precipitation and evapotranspiration distributions for the Pasco Basin for use in groundwater recharge calculations. The results are shown on precipitation and evapotranspiration distribution maps. The parameters, calculation methods, sensitivity determinations, and fitting methods used in the development of these maps are also discussed

  20. The Mediterranean basin

    DEFF Research Database (Denmark)

    Tomas, Carmen; Sanchez Sanchez, Juan Jose; Barbaro, A.;

    2008-01-01

    genetically from the rest of the populations in the Mediterranean area. This result supports the hypothesis of a low incidence of the south-north genetic interchange at the western shores of the Mediterranean basin. A low genetic distance was found between populations in the Middle East and the western part...

  1. Restoring the Nile Basin

    OpenAIRE

    World Bank Group

    2015-01-01

    Watershed management has come to be recognized as a critical issue in the Nile Basin. Upstream land use can cause degradation and soil erosion, resulting in lower agricultural yields locally and causing sedimentation downstream. The increased sediment load causes economic problems by reducing water quality, and irrigation and hydropower potential, as well as increasing flooding. This note ...

  2. Gulf Coast Programmatic Environmental Assessment Geothermal Well Testing: The Frio Formation of Texas and Louisiana

    Energy Technology Data Exchange (ETDEWEB)

    None

    1977-10-01

    In accordance with the requirements of 10 CFR Part 711, environmental assessments are being prepared for significant activities and individual projects of the Division of Geothermal Energy (DGE) of the Energy Research and Development Administration (ERDA). This environmental assessment of geopressure well testing addresses, on a regional basis, the expected activities, affected environments, and possible impacts in a broad sense. The specific part of the program addressed by this environmental assessment is geothermal well testing by the take-over of one or more unsuccessful oil wells before the drilling rig is removed and completion of drilling into the geopressured zone. Along the Texas and Louisiana Gulf Coast (Plate 1 and Overlay) water at high temperatures and high pressures is trapped within Gulf basin sediments. The water is confined within or below essentially impermeable shale sequences and carries most or all of the overburden pressure. Such zones are referred to as geopressured strata. These fluids and sediments are heated to abnormally high temperatures (up to 260 C) and may provide potential reservoirs for economical production of geothermal energy. The obvious need in resource development is to assess the resource. Ongoing studies to define large-sand-volume reservoirs will ultimately define optimum sites for drilling special large diameter wells to perform large volume flow production tests. In the interim, existing well tests need to be made to help define and assess the resource. The project addressed by this environmental assessment is the performance of a geothermal well test in high potential geothermal areas. Well tests involve four major actions each of which may or may not be required for each of the well tests. The four major actions are: site preparation, drilling a salt-water disposal well, actual flow testing, and abandonment of the well.

  3. Bransfield Basin and Cordilleran Orogenesis

    Science.gov (United States)

    Dalziel, I. W.; Austin, J. A.; Barker, D. H.; Christensen, G. L.

    2003-12-01

    Tectonic uplift of the Andean Cordillera was initiated in the mid-Cretaceous with inversion of a composite marginal basin along 7500 km of the continental margin of South America, from Peru to Tierra del Fuego and the North Scotia Ridge. In the southernmost Andes, from 50-56 degrees S, the quasi-oceanic floor of this basin is preserved in the obducted ophiolitic rocks of the Rocas Verdes (Green Rocks) basin. We suggest that the basin beneath Bransfield Strait, 61-64 degrees S, separating the South Shetland Islands from the Antarctic Peninsula, constitutes a modern analog for the Rocas Verdes basin. Marine geophysical studies of Bransfield basin have been undertaken over the past 12 years by the Institute for Geophysics, University of Texas at Austin, under the auspices of the Ocean Sciences Division and United States Antarctic Program, National Science Foundation. These studies have elucidated the structure and evolution of Bransfield basin for comparison with the Rocas Verdes basin, with a view to eventual forward modeling of the evolution of a hypothetical cordilleran orogen by compression and inversion of the basin. These are the processes that can be observed in the tectonic transformation of the Rocas Verdes basin into the southernmost Andean cordillera, as South America moved rapidly westward in an Atlantic-Indian ocean hot-spot reference frame during the mid-Cretaceous. Multi-channel reflection seismic data from the Bransfield basin reveal an asymmetric structural architecture characterized by steeply-dipping normal faults flanking the South Shetlands island arc and gently dipping listric normal faults along the Antarctic Peninsula margin. Normal fault polarity reversals appear to be related to distributed loci of magmatic activity within the basin. This architecture is remarkably similar to that deduced from field structural studies of the Rocas Verdes basin. Notably, the oceanward-dipping, low angle normal faults along the Antarctic Peninsula margin

  4. Seismic Activity in the Gulf of Mexico: a Preliminary Analysis

    Science.gov (United States)

    Franco, S. I.; Canet, C.; Iglesias, A.; Valdes-Gonzales, C. M.

    2013-05-01

    The southwestern corner of Gulf of Mexico (around the northern Isthmus of Tehuantepec) is exposed to an intense deep (> 100 km) seismic activity caused by the subduction of the Cocos plate. Aside from this, the gulf has been considered as a zone of low or no-seismicity. However, a sparse shallow seismic activity is observed across the Gulf of Mexico; some of these earthquakes have been strongly felt (e.g. 23/05/2007 and 10/09/2006), and the Jaltipan, 1959 earthquake caused fatalities and severe destruction in central and southern Veracruz. In this work we analyze 5 relevant earthquakes that occurred since 2001. At the central Gulf of Mexico focal mechanisms show inverse faults oriented approximately NW-SE with dip near 45 degrees, suggesting a link to sediment loading and/or to salt tectonics. On the other hand, in the southwestern corner of the gulf we analyzed some clear examples of strike-slip faults and activity probably related to the Veracruz Fault. One anomalous earthquake, recorded in 2007 in the western margin of the gulf, shows a strike-slip mechanism indicating a transform regime probably related with the East Mexican Fault. The recent improvement of the Mexican Seismological broadband network have allowed to record small earthquakes distributed in and around the Gulf of Mexico. Although the intermediate and large earthquakes in the region are infrequent, the historic evidence indicates that the magnitudes could reach Mw~6.4. This fact could be taken in consideration to reassess the seismic hazard for oil and industrial infrastructure in the region.

  5. Rapid ventilation of the Mexico City basin and regional fate of the urban plume

    Directory of Open Access Journals (Sweden)

    B. de Foy

    2006-01-01

    Full Text Available Urban areas can be large emitters of air pollutants leading to negative health effects and environmental degradation. The rate of venting of these airsheds determines the pollutant loading for given emission levels, and also determines the regional impacts of the urban plume. Mexico City has approximately 20 million people living in a high altitude basin with air pollutant concentrations above the health limits most days of the year. A mesoscale meteorological model (MM5 and a particle trajectory model (FLEXPART are used to simulate air flow within the Mexico City basin and the fate of the urban plume during the MCMA-2003 field campaign. The simulated trajectories are validated against pilot balloon and radiosonde trajectories. The residence time of air within the basin and the impacted areas are identified by episode type. Three specific cases are analysed to identify the meteorological processes involved. For most days, residence times in the basin are less than 12 h with little carry-over from day to day and little recirculation of air back into the basin. Very efficient vertical mixing leads to a vertically diluted plume which, in April, is transported predominantly towards the Gulf of Mexico. Regional accumulation was found to take place for some days however, with urban emissions sometimes staying over Mexico for more than 6 days. Knowledge of the residence times, recirculation patterns and venting mechanisms will be useful in guiding policies for improving the air quality of the MCMA.

  6. Multi-approach quantification of denudation rates in the Gulf of Lion source-to-sink system (SE France)

    Science.gov (United States)

    Molliex, S.; Rabineau, M.; Leroux, E.; Bourlès, D. L.; Authemayou, C.; Aslanian, D.; Chauvet, F.; Civet, F.; Jouët, G.

    2016-06-01

    During the Pliocene and the Quaternary, the Gulf of Lion, the northern passive margin of the Liguro-Provençal basin in the western Mediterranean Sea, received sediments from a 120 000 km2 drainage area constituted by several structural domains. The denudation of mountainous areas, source of this sedimentary supply, results from complex interactions between tectonics, climate, morphology, and rock erodibility. In this study, denudation rates from the present-day and ranging back to the Quaternary and the Pliocene are quantified using four independent methods allowing an investigation over different time scales: 1) compilation of present-day measured sediment fluxes, 2) determination of catchment-scale cosmogenic denudation rates through measurements of in situ-produced 10Be concentrations in sands sampled at the outlet of present-day rivers, 3) estimation of eroded volumes within catchments using a DEM to quantify long-term averaged Quaternary denudation rates, and 4) quantification of sediment volumes deposited within the marine realm of the Gulf of Lion. The results obtained by these four methods are in agreement within the range of uncertainties. The internal part of the Alps exhibits significantly higher denudation rates (∼700 mm ka-1) than those estimated in the other structural domains: 150-250 mm ka-1 in the foreland Alps, ∼100 mm ka-1 in the Pyrenees, and 55-75 mm ka-1 in the Massif Central. The Alpine domain provides at least 80% of the total eroded volume supplied towards the Gulf of Lion. A quantitative geomorphological approach shows that denudation rates are controlled at the first order by catchment morphologies (slope, relief) over different time scales, suggesting glacial conditioning to be the main driver on denudation from the Quaternary to present-day. Throughout the Pliocene-Quaternary, a doubling of denudation rates related to the mid-Pleistocene Revolution (∼0.9 Ma) is highlighted.

  7. 78 FR 59656 - Gulf of Mexico Fishery Management Council; Public Meeting

    Science.gov (United States)

    2013-09-27

    ...The Gulf of Mexico Fishery Management Council (Council) will hold a meeting of its Law Enforcement Advisory Panel in conjunction with the Gulf States Marine Fisheries Commission's Law Enforcement...

  8. 76 FR 61695 - Gulf of Mexico Regional Ecosystem Restoration Strategy (Preliminary)

    Science.gov (United States)

    2011-10-05

    ... AGENCY Gulf of Mexico Regional Ecosystem Restoration Strategy (Preliminary) AGENCY: Environmental... the Gulf of Mexico Regional Ecosystem Restoration Strategy (Preliminary) for public review and... Mexico Ecosystem Restoration Strategy. Additionally, the Task Force was instructed to build upon...

  9. State of oil pollution in the northern Arabian Sea after the 1991 Gulf oil spill

    Digital Repository Service at National Institute of Oceanography (India)

    Sengupta, R.; Fondekar, S.P.; Alagarsamy, R.

    Following the enormous oil spills resulting from the 1990-91 military conflict in the Gulf, fears were expressed concerning dissipation of oil from the Gulf into the Arabian Sea and Indian Ocean. To investigate contamination of the northern Arabian...

  10. Gulf of Mexico dissolved oxygen model (GoMDOM) research and quality assurance project plan

    Science.gov (United States)

    An integrated high resolution mathematical modeling framework is being developed that will link hydrodynamic, atmospheric, and water quality models for the northern Gulf of Mexico. This Research and Quality Assurance Project Plan primarily focuses on the deterministic Gulf of Me...

  11. Stratigraphy of two conjugate margins (Gulf of Lion and West Sardinia): modeling of vertical movements and sediment budgets

    Science.gov (United States)

    Leroux, Estelle; Gorini, Christian; Aslanian, Daniel; Rabineau, Marina; Blanpied, Christian; Rubino, Jean-Loup; Robin, Cécile; Granjeon, Didier; Taillepierre, Rachel

    2016-04-01

    The post-rift (~20-0 Ma) vertical movements of the Provence Basin (West Mediterranean) are quantified on its both conjugate (the Gulf of Lion and the West Sardinia) margins. This work is based on the stratigraphic study of sedimentary markers using a large 3D grid of seismic data, correlations with existing drillings and refraction data. The post-rift subsidence is measured by the direct use of sedimentary geometries analysed in 3D [Gorini et al., 2015; Rabineau et al., 2014] and validated by numerical stratigraphic modelling. Three domains were found: on the platform (1) and slope (2), the subsidence takes the form of a seaward tilting with different amplitudes, whereas the deep basin (3) subsides purely vertically [Leroux et al., 2015a]. These domains correspond to the deeper crustal domains respectively highlighted by wide angle seismic data. The continental crust (1) and the thinned continental crust (2) are tilted, whereas the intermediate crust, identified as lower continental exhumed crust [Moulin et al., 2015, Afhilado et al., 2015] (3) sagged. The post-break-up subsidence re-uses the initial hinge lines of the rifting phase. This striking correlation between surface geologic processes and deep earth dynamic processes emphasizes that the sedimentary record and sedimentary markers is a window into deep geodynamic processes and dynamic topography. Pliocene-Pleistocene seismic markers enabled high resolution quantification of sediment budgets over the past 6 Myr [Leroux et al., in press]. Sediment budget history is here completed on the Miocene interval. Thus, the controlling factors (climate, tectonics and eustasy) are discussed. Afilhado, A., Moulin, M., Aslanian, D., Schnürle, P., Klingelhoefer, F., Nouzé, H., Rabineau, M., Leroux, E. & Beslier, M.-O. (2015). Deep crustal structure across a young 1 passive margin from wide-angle and reflection seismic data (The SARDINIA Experiment) - II. Sardinia's margin. Bull. Soc. géol. France, 186, ILP Spec. issue, 4

  12. Population Structure, Abundance and Movement of Whale Sharks in the Arabian Gulf and the Gulf of Oman.

    Science.gov (United States)

    Robinson, David P; Jaidah, Mohammed Y; Bach, Steffen; Lee, Katie; Jabado, Rima W; Rohner, Christoph A; March, Abi; Caprodossi, Simone; Henderson, Aaron C; Mair, James M; Ormond, Rupert; Pierce, Simon J

    2016-01-01

    Data on the occurrence of whale sharks, Rhincodon typus, in the Arabian Gulf and Gulf of Oman were collected by dedicated boat surveys and via a public-sightings scheme during the period from 2011 to 2014. A total of 422 individual whale sharks were photo-identified from the Arabian Gulf and the northern Gulf of Oman during that period. The majority of sharks (81%, n = 341) were encountered at the Al Shaheen area of Qatar, 90 km off the coast, with the Musandam region of Oman a secondary area of interest. At Al Shaheen, there were significantly more male sharks (n = 171) than females (n = 78; X2 = 17.52, P sharks was 6.90 m ± 1.24 (median = 7 m; n = 296). Males (7.25 m ± 1.34; median = 8 m, n = 171) were larger than females (6.44 m ±1.09; median = 7 m, n = 78; Mann-Whitney U test, p sharks assessed for maturity 63% were mature (n = 81), with 50% attaining maturity by 7.29 m and 100% by 9.00 m. Two female sharks of >9 m individuals were visually assessed as pregnant. Connectivity among sharks sighted in Qatari, Omani and UAE waters was confirmed by individual spot pattern matches. A total of 13 identified sharks were re-sighted at locations other than that at which they were first sighted, including movements into and out of the Arabian Gulf through the Strait of Hormuz. Maximum likelihood techniques were used to model an estimated combined population for the Arabian Gulf and Gulf of Oman of 2837 sharks ± 1243.91 S.E. (95% C.I. 1720-6295). The Al Shaheen aggregation is thus the first site described as being dominated by mature males while the free-swimming pregnant females are the first reported from the Indian Ocean. PMID:27362839

  13. Gulf team delivers on DP drillship promise

    Energy Technology Data Exchange (ETDEWEB)

    Flatern, R. von

    2001-06-01

    The technological achievements of the project by Amoco and BP to complete a deepwater subsea well in the Gulf of Mexico from a dynamically positioned (DP) vessel are described. In 2000, the dual activity drillship, Discoverer Enterprise (owned by Transocean Sedco Forex), completed the Nile well in the Viosca Knoll area and then the King Well in Mississippi Canyon Block 85. Stringent safety and environmental protection criteria imposed by Amoco and BP drove the design of the Dril-Quip subsea wellhead to ensure that the wellhead profile and connector coped with the worst case scenario. BP also specified a disconnect system that would secure the well in less than a minute. The SenTREE 7 and Commander telemetry systems developed by Schlumberger, the components of the work string and test work with the Nile well to ensure BP conditions were met and that the perforation and surge procedure proceeded successfully are explained. The time reduction achieved by using large DP drillships and future BP plans are outlined.

  14. Gulf of Mexico Oceanography Atlas available

    Science.gov (United States)

    The second full-color volume of the Atlas Oceanogáfico del Golfo de México has recently been published by the Grupo de Estudios Oceanográficos of the Instituto de Investigaciones Eléctricas of México (GEO-IIE) (see Eos, Feb. 20, 1990, for announcement of volume 1). This second of an eight-volume series describes the hydrography, baroclinic flows and transports, water masses distributions, and the kinematic properties of anticyclonic-cyclonic ring pairs (modons) of the central and western Gulf of Mexico (26°-20°40‧N, 97°40‧-93°W). The data presented and analyzed in this volume were collected during the Argos 86-1 oceanographic cruise conducted by the GEO-IIE aboard the R/V Justo Sierra during October and November 1986. Authors of the volume are Víctor M. V. Vidal, Francisco V. Vidal, and Abel Hernández. It has 16 chapters in 715 pages, including 248 full-page color plates and 35 tables.

  15. Upwelling characteristics in the Gulf of Finland (Baltic Sea) as revealed by Ferrybox measurements in 2007-2013

    Science.gov (United States)

    Kikas, Villu; Lips, Urmas

    2016-07-01

    Ferrybox measurements have been carried out between Tallinn and Helsinki in the Gulf of Finland (Baltic Sea) on a regular basis since 1997. The system measures autonomously water temperature, salinity, chlorophyll a fluorescence and turbidity and takes water samples for further analyses at a predefined time interval. We aimed to show how the Ferrybox technology could be used to study the coastal upwelling events in the Gulf of Finland. Based on the introduced upwelling index and related criteria, 33 coastal upwelling events were identified in May-September 2007-2013. The number of events, as well as the frequency of their occurrence and intensity expressed as a sum of daily average temperature deviations in the 20 km wide coastal area, were almost equal near the northern and southern coasts. Nevertheless, the wind impulse, which was needed to generate upwelling events of similar intensity, differed between the northern and southern coastal areas. It is suggested that the general thermohaline structure adapted to the prevailing forcing and the estuarine character of the basin weaken the upwelling created by the westerly to southwesterly (up-estuary) winds and strengthen the upwelling created by the easterly to northeasterly (down-estuary) winds. Two types of upwelling events were identified - one characterized by a strong temperature front and the other revealing gradual decrease in temperature from the open sea to the coastal area, with maximum temperature deviation close to the shore.

  16. Detachment Faulting and Hanging-wall Segmentation in the Gulf Extensional Province, Baja California

    Science.gov (United States)

    Seiler, C.; Fletcher, J. M.; Quigley, M. C.; Gleadow, A. J.; Kohn, B. P.

    2007-12-01

    The opening of the Gulf of California, caused by the re-localization of the Pacific -- North America plate boundary, is a premier example of an incipient passive margin. The San Felipe area in northern Baja California comprises a typical basin and range-style topography, produced by Neogene extension affecting the Gulf Extensional Province (GEP). The > 100 km long Sierra San Pedro Mártir (SSPM) escarpment is defined by an east-down normal fault system, separating the unextended western part of the peninsula from the GEP. The hanging-wall of the SSPM fault is characterized by several fault-bound blocks that have been rotated around both vertical and horizontal axes. The Las Cuevitas and the Santa Rosa detachments are two major fault systems in the Sierra San Felipe that are responsible for segmentation of the hanging-wall of the SSPM fault. The curvilinear, NE to NNW striking Las Cuevitas Detachment extends for more than 43 km and brings Neogene volcanics and sediments in contact with the Mesozoic basement of the footwall. The detachment dips at 15-50° and accommodates more than 4-6 km of east-down displacement. Faulting appears to preferentially occur at the contact of Mesozoic metamorphics to granitoid intrusives with transfer faults translating deformation between the faulted contacts. Fission track and (U-Th)/He thermochronology constrain the initiation of deformation on the Las Cuevitas detachment to the latest Miocene. The > 45 km long and equally curvilinear Santa Rosa Detachment system consists of a low-angle normal fault system (15-35° dip) with transfer zones facilitating the transfer of strain between individual segments of the detachment fault. The slip direction varies between top-to-the-east and top-to-the-south, a possible explanation for the change in strike from NW to NE to NW. The roughly 4-5 km offset of Neogene volcanic and sedimentary deposits has created the necessary space for syntectonic deposition in the Santa Rosa Basin. The onset of

  17. Archeterokrohnia docrickettsae (Chaetognatha: Phragmophora: Heterokrohniidae), a new species of deep-sea arrow worm from the Gulf of California.

    Science.gov (United States)

    Thuesen, Erik V; Haddock, Steven H D

    2013-01-01

    A new species of deep-sea chaetognath, Archeterokrohnia docrickettsae n. sp. is described from a single specimen captured by the ROV Doc Ricketts ~2 m above the sea floor at 3245 m depth in the Pescadero Basin of the Gulf of California, Mexico. This is the first record of a living specimen of Archeterokrohnia and the second known occurrence of Archeterokrohnia in the Pacific Ocean. In life, the head and trunk sections were orange, while the tail section was translucent, a unique colour pattern not before seen in chaetognaths. Observations of its swimming behaviour in situ are given. Comparisons are made with the three other species of Archeterokrohnia. At 28.5 mm in length, this is the largest known species of the genus. An artificial key to the four species of Archeterokrohnia is presented. PMID:26176108

  18. Mapping the Intricacies of the Gulf of Mexico's Circulation

    Science.gov (United States)

    Lugo-Fernández, Alexis; Green, Rebecca E.

    2011-01-01

    From hosting key shipping lines, drilling platforms, and commercial fisheries, to sustaining mangrove swamps that shelter the coastline from the hurricanes that churn its waters, the Gulf of Mexico is important to the nations surrounding it for socio-economic, ecological, military, political, and scientific reasons. Critical to all of these sectors is the Gulf's circulation—it controls hurricane tracks and intensity, biological productivity, and larvae dispersal. Since 1982, the Environmental Studies Program (ESP) of the U.S. Bureau of Ocean Energy Management, Regulation and Enforcement (BOEMRE) has invested more than $67 million in field and numerical modeling studies to improve our understanding of the Gulf's circulation (see Figure 1). ESP-funded research has covered a broad array of topics, some applied and some basic. Studies carried out on behalf of the bureau reflect the bureau's information needs, stakeholder input, and offshore energy exploration and development trends. All ESP studies culminate in a technical report—127 technical reports on physical oceanography are publicly available (see http://www.gomr.boemre.gov/homepg/regulate/environ/techsumm/rec_pubs.html). Additionally, more than 100 peer-reviewed publications have been issued on the Gulf's physical oceanography and circulation. The AGU Geophysical Monograph Circulation in the Gulf of Mexico: Observations and Models, the very first circulation overview since 1972, was funded by ESP. Additionally, data collected during fieldwork are deposited in national archives for public dissemination.

  19. Inshore/offshore water exchange in the Gulf of Naples

    Science.gov (United States)

    Cianelli, Daniela; Falco, Pierpaolo; Iermano, Ilaria; Mozzillo, Pasquale; Uttieri, Marco; Buonocore, Berardino; Zambardino, Giovanni; Zambianchi, Enrico

    2015-05-01

    The Gulf of Naples is a coastal area in the south-eastern Tyrrhenian Sea (western Mediterranean). Zones of great environmental and touristic value coexist in this area with one of the largest seaports in the Mediterranean Sea, industrial settlements and many other pollution sources. In such an environment, water renewal mechanisms are crucial for maintaining the ecological status of the coastal waters. In this paper, we focus on the water exchange between the interior of the Gulf and the neighbouring open Tyrrhenian Sea. The surface dynamics of the Gulf have been investigated based on measurements carried out with a high-frequency (HF) radar system. The vertical component of the current field has been provided by the Regional Ocean Modelling System (ROMS) model of ocean circulation. We present the results of a one-year-long analysis of data and simulation results relative to the year 2009. Inshore/offshore exchanges were assessed by looking at the zonal component of the surface and subsurface current field across a transect representing a sort of threshold between the interior of the Gulf and the open sea. This also allows for the reconstruction of the short-term origin of waters found inside the Gulf in the different forcing and circulation conditions.

  20. Preliminary observations of environmental damage due to the Gulf War

    International Nuclear Information System (INIS)

    Preparing for and conducting the Gulf War resulted in much damage to the environment of the region. The first and most visible effect is related to the damage caused by oil well fires in terms of air pollution as well as the potential damage to the petroleum reservoirs. The second detrimental effect has been caused by the oil spill in the Gulf water. Hundreds of miles of the western coastline of the Gulf are already covered with oil. Petroleum 'mats' have settled on coral reefs and have reduced Gulf water productivity. Foremost among the irreparable damages are changes to the terrain due to the digging of trenches, building walls of soil and otherwise disturbing the desert pavement in and around Kuwait. Disruption of the, usually, one-grain thick layer of pebbles on the desert floor exposes soil to wind action. Changing the contours of the normally flat land increases resistance to the wind and increases the potential of particle transport until the land is peneplained. This condition will increase the frequency and the ferocity of dust storms in the region. It will also result in the formation of new sand dunes; sand drifts already exist along roads in northern Kuwait. It is believed that the detrimental effects on the atmosphere will last for years, on the Gulf water for decades, and on the desert surface for centuries. (author). 12 refs, 1 fig

  1. Petroleum exploration potential of Tamtsag Basin

    Institute of Scientific and Technical Information of China (English)

    SUN Guo-qing; GUO Qing-xia; ZHANG Ya-jin; ZHAO Hong-wen

    2004-01-01

    The Tamtsag Basin is located in the extreme eastern portion of the Mongolia. The Basin and its counterpart in China (the Hailar Basin) are united a whole basin on the structural setting. In recent years, the Tamtsag Basin attracts more and more attention with the important exploration discovered in the 19th block by SOCO and in Hailar Basin of China. This paper discusses the exploration potential of Tamtsag Basin from the viewpoint of petroleum geology.

  2. Africa and Arab Gulf states : Divergent Development Paths and Prospects for Convergence

    OpenAIRE

    Fofack, Hippolyte

    2009-01-01

    In spite of the similarities between Sub-Saharan Africa and the Arab Gulf region (Gulf Cooperation Council states), development policies implemented in these two regions of the world have produced markedly different and even divergent outcomes. While Gulf Cooperation Council states have drawn on hydrocarbon revenues to dramatically transform their economic landscape, Sub-Saharan African co...

  3. The consequences and hazards of depleted uranium weapons used by US army since gulf war

    International Nuclear Information System (INIS)

    Military equipment and development of depleted uranium weapon in USA, the depleted uranium weapon used in gulf war by USA army, personnel irradiation in the gulf war, and the protection in the gulf war are introduced. The radioactivity, radioactive characteristics, chemical toxicity and hazard of the depleted uranium are also introduced

  4. 78 FR 4130 - Gulf of Mexico Fishery Management Council; Public Meetings

    Science.gov (United States)

    2013-01-18

    ... Offshore Marine Aquaculture in the Gulf of Mexico. 9:30 a.m.-9:45 a.m.--The Council will vote on Exempted... National Oceanic and Atmospheric Administration RIN 0648-XC449 Gulf of Mexico Fishery Management Council... Administration (NOAA), Commerce. ACTION: Notice of public meetings. SUMMARY: The Gulf of Mexico...

  5. Observing environmental change in of the Gulf of Maine: ICUC smartphone app

    Science.gov (United States)

    Want to help collect data on environmental change in the Gulf of Maine with your smartphone? The Gulf of Maine Council’s EcoSystem Indicator Partnership (ESIP) is growing the community of citizen scientists in the Gulf of Maine region through its new smartphone app: ICUC (...

  6. 75 FR 69921 - Gulf of Mexico Fishery Management Council; Public Meetings

    Science.gov (United States)

    2010-11-16

    ... process, the Gulf of Mexico Alliance Regional Sediment Management Plan, and the Essential Fish Habitat 5... National Oceanic and Atmospheric Administration RIN 0648-XA027 Gulf of Mexico Fishery Management Council... Administration (NOAA), Commerce. ACTION: Notice of public meetings. SUMMARY: The Gulf of Mexico...

  7. Syn-rift volcanism and seafloor-spreading in the northern Gulf of Mexico: results from the GUMBO marine seismic refraction project

    Science.gov (United States)

    Eddy, D. R.; Van Avendonk, H. J.; Christeson, G. L.; Norton, I. O.; Karner, G. D.; Kneller, E. A.; Johnson, C. A.; Snedden, J.

    2013-12-01

    Continental rifting and seafloor-spreading between North America and the Yucatán Block during the Jurassic to early Cretaceous formed the small ocean basin known today as the Gulf of Mexico. The lack of deeply-penetrating geophysical data in the Gulf of Mexico limited early reconstructions of the timing and location of the rift-to-drift transition, particularly with respect to the influence of magmatism on the breakup of continental crust and the onset of seafloor-spreading. To better understand the deep structure of this economically important basin, we acquired four marine seismic refraction profiles in the northern Gulf of Mexico from the shelf to deep water as part of the 2010 Gulf of Mexico Basin Opening project (GUMBO). We use travel times from long-offset reflections and refractions to image compressional seismic velocities in the sediments, crystalline crust, and upper mantle using an iterative tomographic inversion. GUMBO Line 3 extends from offshore Alabama through the De Soto Canyon towards the central Gulf of Mexico. We interpret velocities >5.0 km/s in the sediment layer landward of the Florida Escarpment as a Lower Cretaceous carbonate platform. Crystalline crust with velocities between 5.5-7.5 km/s thins significantly from 23 km to 7 km across a narrow necking zone. A deep, localized region of anomalously high seismic velocities (>7.5 km/s) at the base of crystalline crust exceeds those of continental lower crust in the eastern US. We interpret this section of GUMBO 3 to represent mafic under-plating and/or infiltration of asthenospheric melts, common at volcanic rifted margins. The seaward end of GUMBO 3 has seismic velocities consistent with mafic ocean crust produced by normal seafloor-spreading (6.0-7.5 km/s); this observation is supported by a consistent crustal thickness of ~7 km and minimal lateral heterogeneities in velocity structure. GUMBO Line 2 extends from offshore Louisiana southward across the Sigsbee Escarpment. We find a massive

  8. Canterbury Basin Sea Level

    OpenAIRE

    Fulthorpe, C. S.; Institute for Geophysics John A. and Katherine G. Jackson School of Geosciences The University of Texas at Austin J.J. Pickle Research Campus, Building 196 (ROC) 10100 Burnet Road (R2200) Austin TX 78758-4445 USA; Hoyanagi, K.; Department of Geology Faculty of Science Shinshu University 3-1-1 Asahi, Matsumoto 390-8621 Japan; Blum, P.; United States Implementing Organization Integrated Ocean Drilling Program Texas A&M University 1000 Discovery Drive College Station TX 77845 USA; Guèrin, G.; Borehole Research Group Lamont-Doherty Earth Observatory of Columbia University PO Box 1000, 61 Route 9W Palisades NY 10964 USA; Slagle, A. L.; Borehole Research Group Lamont-Doherty Earth Observatory of Columbia University PO Box 1000, 61 Route 9W Palisades NY 10964 USA; Blair, S. A.; Department of Geological Sciences Florida State University 006 Carraway Building Tallahassee FL 32306 USA; Browne, G. H.; Hydrocarbon Section GNS Science PO Box 30368 Lower Hutt New Zealand; Carter, R. M.; Marine Geophysical Laboratory James Cook University of North Queensland Townsville QLD 4811 Australia; Ciobanu, M.; Laboratoire de Microbiologie des Environnements Extrêmes CNRS UMR-6197 Institut Universitaire Européen de la Mer Technopole Brest-Iroise Plouzane 29280 France; Claypool, G. E.; Organic Geochemist 8910 West 2nd Avenue Lakewood CO 80226 USA; Crundwell, M. P.; New Zealand Observer/Paleontologist (foraminifers) Paleontology and Environmental Change Section GNS Science PO Box 30368 Lower Hutt New Zealand; Dinarès-Turell, J.; Istituto Nazionale di Geofisica e Vulcanologia, Sezione Roma2, Roma, Italia; Ding, X.; School of Marine Sciences China University of Geosciences (Beijing) 29 XueYuan Road, Haidian District Beijing P.R. China; George, S. C.; Department of Earth and Planetary Sciences Macquarie University Sydney NSW 2109 Australia; Hepp, D. A.; MARUM – Center for Marine Environmental Sciences and Department of Geosciences University of Bremen Leobener Strasse MARUM Building, Room 2230 28359 Bremen Germany

    2010-01-01

    Integrated Ocean Drilling Program (IODP) Expedition 317 was devoted to understanding the relative importance of global sea level (eustasy) versus local tectonic and sedimentary processes in controlling continental margin sedimentary cycles. The expedition recovered sediments from the Eocene to recent period, with a particular focus on the sequence stratigraphy of the late Miocene to recent, when global sea level change was dominated by glacioeustasy. Drilling in the Canterbury Basin,...

  9. Lakes of the Huron basin: their record of runoff from the laurentide ice sheet

    Science.gov (United States)

    Michael Lewis, C. F.; Moore, Theodore C.; Rea, David K.; Dettman, David L.; Smith, Alison M.; Mayer, Larry A.

    The 189,000 km2 Huron basin is central in the catchment area of the present Laurentian Great Lakes that now drain via the St. Lawrence River to the North Atlantic Ocean. During deglaciation from 21-7.5 ka BP, and owing to the interactions of ice margin positions, crustal rebound and regional topography, this basin was much more widely connected hydrologically, draining by various routes to the Gulf of Mexico and Atlantic Ocean, and receiving overflows from lakes impounded north and west of the Great Lakes-Hudson Bay drainage divide. Early ice-marginal lakes formed by impoundment between the Laurentide Ice Sheet and the southern margin of the basin during recessions to interstadial positions at 15.5 and 13.2 ka BP. In each of these recessions, lake drainage was initially southward to the Mississippi River and Gulf of Mexico. In the first recession, drainage subsequently switched eastward along the ice margin to the North Atlantic Ocean. In the second recession, drainage continued southward through the Michigan basin, and later, eastward via the Ontario basin and Mohawk River valley to the North Atlantic Ocean. During the final retreat of ice in the Huron basin from 13 to 10 ka BP, proglacial lake drainage switched twice from the Michigan basin and the Mississippi River system to the North Atlantic via the Ontario basin and Mohawk River valley, finally diverting to the Champlain Sea in the St. Lawrence River valley at about 11.6 ka BP. New seismo- and litho-stratigraphic information with ostracode data from the offshore lacustrine sediments were integrated with the traditional data of shorelines, uplift histories of outlets, and radio-carbon-dated shallow-water evidence of transgressions and regressions to reconstruct the water level history and paleolimnological record for the northern Huron basin for the 11-7 ka BP period. Negative excursions in the δ18O isotopic composition of ostracodes and bivalves in southern Lake Michigan, southwestern Lake Huron and eastern

  10. Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska

    Science.gov (United States)

    Plafker, George; Addicott, W.O.

    1976-01-01

    Perhaps the world's longest and most complete onshore sedimentary record of late Cenozoic glaciation is preserved in the Gulf of Alaska Tertiary province that extends 800 km along the coast of southern Alaska. The Yakataga Formation, with an aggregate outcrop thickness of about 5,000 m, is characterized by variable amounts of distinctive neritic marine tillite-like diamictite and laminated siltstone containing dropstones interpreted as ice-rafted glacial debris. The lithology, sedimentary structures and molluscan fauna of the formation suggest that active tidal glaciers or an ice shelf were present along the landward margin of the basin possibly beginning in early or early middle Miocene time. Dropstone distribution in outcrop sections indicates that glaciers reached tidewater intermittently during the Miocene and were almost continually present throughout the Pliocene and much of the Pleistocene. Paleomagnetic and nannoplankton dating of the upper 1,181 m of the Yakataga Formation at Middleton Island indicate that this part of the sequence probably was entirely deposited during the Matuyama reversed polarity epoch of the Pleistocene during which the sedimentation rate was of the order of 1 m/1,000 years. Lithologically similar deposits of poorly consolidated sandy mud and pebbly mud continue to accumulate locally near tidal glaciers in the same area, and older late Quaternary deposits are undoubtedly present offshore. The anomalous late Cenozoic glaciation recorded in the sediments along the Gulf of Alaska margin reflects a fortuitous combination of a subsiding shelf basin adjacent to an area of extremely high elevations and exceptionally heavy precipitation, an environment that persists to the present.

  11. Uranium and other natural radionuclides in the sediments of a Mediterranean fjord-like embayment, Amvrakikos Gulf (Ionian Sea), Greece.

    Science.gov (United States)

    Papaefthymiou, H; Athanasopoulos, D; Papatheodorou, G; Iatrou, M; Geraga, M; Christodoulou, D; Kordella, S; Fakiris, E; Tsikouras, B

    2013-08-01

    The distribution of the natural radionuclides ((238)U, (232)Th, (226)Ra, (40)K) and the artificial (137)Cs was studied in sediment cores collected from Amvrakikos Gulf, a seasonal anoxic marine basin, using γ-ray spectrometry. The activity of radionuclides, along with the concentrations of Fe and Mn, were also studied in relation to the total organic carbon and the granulometric fractions of the sediments. The results obtained revealed higher (238)U activity concentrations in all the examined sediment samples compared to the world and Greek average values for soil. The high activity values of (238)U are attributed, besides the lattice-held fraction, to phosphate fertilizer inputs in the Gulf via major rivers and/or to alteration processes of phosphate ores located mainly in the drainage basin of the river Louros. The elevated activity values of (40)K could be attributed to the mineralogical composition of the sediments and to phosphate fertilizers containing potassium. Organic matter seems to be a more efficient sorbent for U than clay minerals and amorphous Fe and Mn-oxyhydroxides. Scanning electron microscopy, together with qualitative analysis of some smectites, reveals the occurrence of U, suggesting a limited absorption of U onto clay minerals. The applied BCR sequential extraction procedure revealed that U was found mainly in the refractory phase or associated with organic matter and to a lesser extent as surface-coating oxides, with the exception of one sediment core which is characterized by high content of fresh marine organic matter and presents high percentage of U in the exchangeable fraction. PMID:23538023

  12. A Novel Approach to River Basin Management that Utilizes a Multi-Day Forum to Educate Stakeholders

    Science.gov (United States)

    Langston, M. A.

    2015-12-01

    Large scale river basin management has long been a challenging task. Stakeholder involvement has often been posited as a means to provide a broad base of input and support for management decisions. This has been successful in some situations and not in others. The Desert Landscape Conservation Cooperative (LCC) has proposed a novel approach to large scale watershed management for conservation purposes by stakeholders. This approach involves conducting a multi-day stakeholder forum to gather interested parties, provide them science-based information about the watershed, and solicit their input regarding the research and management needs within the basin. Included within this forum is a Water Tournament patterned after those being developed by the U.S. Army Corps of Engineers' Institute for Water Resources. These tournaments bring stakeholders (such as the various water users, agencies, conservation organizations, and others) in small teams that develop watershed management scenarios (within appropriate constraints) that are then judged based on their merit for addressing the various issues within the basin. These tournaments serve to educate participants and to sensitize them to the perspectives of other participants. Another goal of the forum is to recruit a representative group of stakeholders who will provide guidance for further research to meet the basins management needs. The South Central Climate Science Center (SC CSC) has partnered with the Desert, Southern Rockies, Gulf Coast Prairie, Great Plains, and Gulf Coastal Plains and Ozarks LCCs to implement this approach in the Rio Grande and the Red River Basins. The LCCs are well positioned to convene stakeholders from across political boundaries and throughout these basins. The SC CSC's roles will be providing leadership, funding climate science for the effort, and evaluating the effectiveness of the forum-centered approach.

  13. Analysis Of Zapotec Ceramics Of The Caxonos River Basin, Oaxaca, Mexico By Thermoluminescence (Tl)

    Science.gov (United States)

    Ramirez, A.; Schaaf, P.; Ortiz, E.

    One of the most common materials that appear in archaeological excavations is the ceramics. Ceramic is an evidence for different activities and cultural periods. Thermoluminescence (TL) has been shown to be a very effective method for dating of archaeological ceramics. In this paper, we present the results of 18 Zapotec ceramics from different archaeological sites of the Caxonos River Basin, Northern Sierra of Oaxaca, Mexico, analyzed by TL. Based on these results, we established the first chronological data set of this important Mesoamerica site. Our new data give evidence for the existence of a trade route through the Caxonos River Basin used since 500 AD between the central valley of Oaxaca and the Gulf of Mexico. Methodologically we used the fine grain technique (4-11μm) and for the determination of the paleodose the additive method was applied.

  14. Late differentiation of proximal and distal margins in the Gulf of Aden

    Science.gov (United States)

    Bache, F.; Leroy, S.; D'Acremont, E.; Autin, J.; Watremez, L.; Rouzo, S.

    2009-04-01

    Non-volcanic passive margins are usually described in three different domains (Boillot et al., 1988), namely (1) the continental domain, where the basement is structured in a series of basins and basement rises, (2) the true oceanic domain, where the bathymetry is relatively smooth, and (3) in between them, a transitional domain referred to as the oceanic-continental transition (OCT), where the basement is partly composed of exhumed mantle. The Gulf of Aden is a young and narrow oceanic basin formed in Oligo-Miocene time between the rifted margins of the Arabian and Somalian plates. The distal margin and particularly the OCT domain were previously studied considering a large set of data (Leroy et al., 2004; d'Acremont et al., 2005; d'Acremont et al., 2006; Autin, 2008). This study focalises on the sedimentary cover identified on seismic reflexion profiles acquired during Encens-Sheba (2000) and Encens (2006) cruises. Sedimentary stratal pattern and seismic facies succession suggest that the differentiation between the proximal and the distal margins occurred very late in the formation of the margin, after the deposition of ~2 km of "syn-OCT" sediments which filled the distal margin grabens. A high position of the proximal and distal margins during rifting and "syn-OCT" sediments deposition could be proposed. The major implication of this evolution should be a shallow nature of "syn-OCT" deposits. The lack of boreholes doesn't permit to affirm this last point. Comparable observations have been described on other passive margins (Moulin, 2003; Moulin et al., 2005; Labails, 2007; Aslanian et al., 2008; Bache, 2008). For some authors, it shows the persistence of a deep thermal anomaly during the early history of the margin (Steckler et al., 1988; Dupré et al., 2007). These observations could be a common characteristic of passive margins evolution and are of major interest for petroleum exploration. Aslanian, D., M. Moulin, O. J.L., P. Unternehr, F. Bache, I. Contrucci

  15. Decadal changes in Gulf of Alaska upwelling source waters

    Science.gov (United States)

    Pozo Buil, Mercedes; Di Lorenzo, Emanuele

    2015-03-01

    Decadal changes in sea surface temperature (SST) in the Gulf of Alaska are linked to long-term transitions in the marine ecosystem. While previous studies have identified the atmospheric variability of the Aleutian Low as an important driver of Ekman pumping and low-frequency SST anomalies, the role of subsurface gyre-scale dynamics remains unexplored. Using a set of reanalysis data sets from 1958 to the present, we find that subsurface temperature anomalies generated along the North Pacific Current significantly contribute through mean upwelling to decadal changes of SST in the Gulf of Alaska. This influence is comparable to the contribution associated with variations in atmospheric winds. Given the exceptional low-frequency character of the propagation of subsurface anomalies (e.g., multidecadal) along the gyre, monitoring subsurface temperature anomalies up stream along the North Pacific Current may enhance the decadal predictability of SST in the Gulf of Alaska and its impact on local marine ecosystems.

  16. Habitat and behaviour of yellowfin tuna Thunnus albacares in the Gulf of Mexico determined using pop-up satellite archival tags.

    Science.gov (United States)

    Weng, K C; Stokesbury, M J W; Boustany, A M; Seitz, A C; Teo, S L H; Miller, S K; Block, B A

    2009-05-01

    This study presents the first data on movement, habitat use and behaviour for yellowfin tuna Thunnus albacares in the Atlantic Basin. Six individuals were tracked in the Gulf of Mexico using pop-up satellite archival tags. Records up to 80 days in length were obtained, providing information on depth and temperature preferences as well as horizontal movements. Thunnus albacares in the Gulf of Mexico showed a strong preference for the mixed layer and thermocline, consistent with findings for this species in other ocean basins. Fish showed a diel pattern in depth distribution, remaining in surface and mixed layer waters at night and diving to deeper waters during the day. The vertical extent of T. albacares habitat appeared to be temperature limited, with fish generally avoiding waters that were >6 degrees C cooler than surface waters. The vertical and thermal habitat usage of T. albacares differs from that of bigeye Thunnus obesus and bluefin Thunnus thynnus, Thunnus orientalis and Thunnus maccoyii tunas. These results are consistent with the results of earlier studies conducted on T. albacares in other oceans. PMID:20735644

  17. Deep-water northern Gulf of Mexico hydrocarbon plays

    International Nuclear Information System (INIS)

    The geologic setting in the deep-water (depths greater than 1,500 feet) Gulf of Mexico is very favorable for the existence of large, commercial hydrocarbon accumulations. These areas have active salt tectonics that create abundant traps, underlying mature Mesozoic source rocks that can be observed expelling oil and gas to the ocean surface, and good quality reservoirs provided by turbidite sand deposits. Despite the limited amount of drilling in the deep-water Gulf of Mexico, 11 deep-water accumulations have been discovered which, when developed, will rank in the top 100 largest fields in the Gulf of Mexico. Proved field discoveries (those with announced development plans) have added over 1 billion barrels of oil equivalent to Gulf of Mexico reserves, and unproved field discoveries may add to additional billion barrels of oil equivalent. The Minerals Management Service, United States Department of the Interior, has completed a gulf-wide review of over 1,086 oil and gas fields and placed every pay sand in each field into a hydrocarbon play (plays are defined by chronostratigraphy, lithostratigraph, structure, and production). Seven productive hydrocarbon plays were identified in the deep-water northern Gulf of Mexico. Regional maps illustrate the productive limits of each play. In addition, field data, dry holes, and wells with sub-economic pay were added to define the facies and structural limits for each play. Areas for exploration potential are identified for each hydrocarbon play. A type field for each play is chosen to demonstrate the play's characteristics

  18. Reproductive health and pregnancy outcomes among French gulf war veterans

    Directory of Open Access Journals (Sweden)

    Bégassat Marion

    2008-04-01

    Full Text Available Abstract Background Since 1993, many studies on the health of Persian Gulf War veterans (PGWVs have been undertaken. Some authors have concluded that an association exists between Gulf War service and reported infertility or miscarriage, but that effects on PGWV's children were limited. The present study's objective was to describe the reproductive outcome and health of offspring of French Gulf War veterans. Methods The French Study on the Persian Gulf War (PGW and its Health Consequences is an exhaustive cross-sectional study on all French PGWVs conducted from 2002 to 2004. Data were collected by postal self-administered questionnaire. A case-control study nested in this cohort was conducted to evaluate the link between PGW-related exposures and fathering a child with a birth defect. Results In the present study, 9% of the 5,666 Gulf veterans who participated reported fertility disorders, and 12% of male veterans reported at least one miscarriage among their partners after the PGW. Overall, 4.2% of fathers reported at least one child with a birth defect conceived after the mission. No PGW-related exposure was associated with any birth defect in children fathered after the PGW mission. Concerning the reported health of children born after the PGW, 1.0% of children presented a pre-term delivery and 2.7% a birth defect. The main birth defects reported were musculoskeletal malformations (0.5% and urinary system malformations (0.3%. Birth defect incidence in PGWV children conceived after the mission was similar to birth defect incidence described by the Paris Registry of Congenital Malformations, except for Down syndrome (PGWV children incidence was lower than Registry incidence. Conclusion This study did not highlight a high frequency of fertility disorders or miscarriage among French PGW veterans. We found no evidence for a link between paternal exposure during the Gulf War and increased risk of birth defects among French PGWV children.

  19. Shrimp Farms and Mangroves, Gulf of Fonseca

    Science.gov (United States)

    2002-01-01

    For decades, astronauts on space missions have documented land use changes around the world. In this pair of images, astronauts track the development of shrimp farming along the Honduran coastline of the Gulf of Fonseca between 1989 and 2001. Mariculture, primarily shrimp farming, has become a leading agricultural effort in Honduras. The regional transformation of large tracts of coastal swamps into shrimp farms blossomed throughout the 1990s. The top image was taken with color infrared film in 1989. Dense vegetation, like the coastal mangrove swamps and the forested slopes of Volcan Cosiguina show up as dark red. The bottom image, taken with color visible film by the crew of the most recent Space Shuttle mission in December 2001 shows that hundreds of square kilometers of coastal swamp, primarily in Honduras, have been converted to shrimp ponds. These appear as the light-colored, rectilinear land use pattern. The Honduras shrimp farms were hit hard by flooding after Hurricane Mitch in 1998, and a devastating virus in 1999-2000. It is not known how many of the ponds in this view are still functional. A vigorous debate continues about the sustainability of the shrimp farms and the impacts to the environment and coastal ecosystem due to mangrove clearing and mariculture waste production. Apart from the shrimp farms, the other prominent feature on these images is the impressive volcano Cosiguina, which erupted explosively in 1859 (the largest recorded eruption in the Western Hemisphere). Photograph STS-108-717-85 was taken in the December 2001 by the crew of Space Shuttle mission 108 using a Hasselblad camera with 250-mm lens. Photograph STS030-93-15 was taken in May 1989 using a Hasselblad camera and color infrared film. Both images are provided by the Earth Sciences and Image Analysis Laboratory at Johnson Space Center. Additional images taken by astronauts and cosmonauts can be viewed at the NASA-JSC Gateway to Astronaut Photography of Earth.

  20. 78 FR 76807 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Revisions to Dealer Permitting...

    Science.gov (United States)

    2013-12-19

    ...The Gulf of Mexico (Gulf) and South Atlantic Fishery Management Councils (Councils) have submitted a Generic Amendment to the Fishery Management Plans (FMPs) in the Gulf and South Atlantic Regions (Generic Dealer Amendment) for review, approval, and implementation by NMFS. The Generic Dealer Amendment amends the following FMPs: Reef Fish Resources and the Red Drum Fishery of the Gulf; the......

  1. Miocene sedimentation and subsidence during continent-continent collision, Bengal basin, Bangladesh

    Science.gov (United States)

    Uddin, Ashraf; Lundberg, Neil

    2004-02-01

    The Bengal basin, a complex foreland basin south of the eastern Himalayas, exhibits dramatic variability in Neogene sediment thickness that reflects a complicated depositional and tectonic history. This basin originally formed as a trailing margin SE of the Indian continental crust, complicated by convergence with Asia to the north and oblique convergence with Burma to the east. Newly compiled isopach data and previously reported seismic data show evidence of thickening of basin fill toward the south, opposite of the pattern typically seen in foreland basins. This is presumably due to sedimentary loading of voluminous deltaic sediments near the continent-ocean boundary and basinward downfaulting analogous to that in the Gulf of Mexico. Isopach data show that there is considerable vertical relief along the base of the Miocene stratigraphic sequence, probably due to down-to-the-basin faulting caused by focused deltaic sedimentation and associated crustal flexure. In contrast, when viewed in east-west profile, basin shape is more typical of a foreland basin, with strata thickening eastward toward the Indo-Burman ranges, which reflects east-west convergence with Southeast Asia. Comparison of the lateral and vertical extent of the Bhuban and Boka Bil Formations with the Bouguer anomaly map of Bangladesh suggests that considerable subsidence of the Sylhet trough (in the northeastern part of the Bengal basin), which has the lowest gravity value of the region, had not taken place by the end of the Miocene. This post-Miocene subsidence is attributed to tectonic loading from southward thrusting of the Shillong Plateau along the Dauki fault. Relatively uniform Miocene isopachs across the Sylhet trough confirm that this began in the Pliocene, consistent with results of recent research on sediment provenance. In the northwest, in the region south of the Siwalik foreland basin, continental crust has not as yet been loaded, allowing relatively little accommodation space for

  2. Oil and gas, strategic regional cooperation between Persian Gulf countries

    Energy Technology Data Exchange (ETDEWEB)

    Zalloi, Mir Mahdi

    2010-09-15

    Almost two-thirds of proven oil and a third of world natural gas resources are in the Persian Gulf countries. Unfortunately strategic region of Persian Gulf in the past three decades faced with many security challenges due to wars and political conflicts. For security in this region, there are several methods such as military treaties between regional countries or Military presence of foreign countries, but historical evidence has shown, none of them could not guarantee the stable security in this region. The regional cooperation between countries can be replaced to mentioned methods. IPI Gas pipeline is an objective sample for this regional cooperation.

  3. Remote Sensing of Suspended Sediment Over Gulf of Martaban

    OpenAIRE

    Matamin Abd Rahman; Ahmad Fadhli; Mamat Mustafa; Abdullah Khiruddin; Harun Shahariah

    2015-01-01

    Gulf of Martaban is located at the north of Andaman, and is one of the world most turbid areas. The presence of suspended sediment concentration (SSC) in the water body could reduce the underwater transmittance. This study has been conducted to investigate the variation of SSC over the Gulf of Martaban. Remote sensing reflectance (Rrs) of 667 nm is used as a proxy to represent the sediment SSC variation over the study area. The data for the period of July 2002 to March 2014 acquired from MODI...

  4. Viscosity correlations for Gulf of Mexico crude oils

    Energy Technology Data Exchange (ETDEWEB)

    Petrosky, G.E. Jr.; Farshad, F.F. [Univ. of Southwestern Louisiana, Lafayette, LA (United States)

    1995-12-31

    In 1984, Sutton and Farshad evaluated the accuracy of several published viscosity correlations for application in the Gulf of Mexico. A total of 31 different crude oil systems from the Louisiana and Texas gulf coast were used in their analysis. The errors encountered were rather high for dead and saturated oil viscosity. New empirical viscosity correlations for estimating dead oil, saturated oil and undersaturated oil viscosities have been developed as a function of commonly available field data. Results show that these viscosities can be predicted with average absolute errors ranging from 2.91% for undersaturated oil viscosity to 14.47% for saturated oil viscosity.

  5. Cities within Cities: An Urbanization Approach in the Gulf Countries

    OpenAIRE

    Bamakhrama, Salim Salah

    2015-01-01

    Within Dubai, nineteen out of the original 112 mega-projects carried the word city in their names, a phenomenon that is common in Gulf cities such as Dubai, Riyadh and Abu Dhabi. To further explore this phenomenon, this thesis focuses on three aspects that affect the dynamic relationship between the primary city and the cities within cities (sub-cities) in the Gulf region with special emphasis on Dubai. First, the naming problem of the sub-city illustrates why the tension between competing id...

  6. Strontium-90 in the western Gulf of Mexico

    International Nuclear Information System (INIS)

    The results of measurements of 90Sr in water, coral, hermit crabs and molluscs from the western Gulf of Mexico and in fresh water molluscs from Canyon Lake, Texas are reported. Preparation of samples for measurement in the anticoincidence mode in a lead shielded flow proportional counter is described. The measured value of 0.095 +- 0.003 pCi/litre for Gulf water is in accord with literature values. Concentration factors for 90Sr are apparently 1 for coral. The activity incorporated into shells normalized to calcium content, decreases from Galveston to Campeche Bay. (U.K.)

  7. Education in the Gulf Monarchies: Retrospect and Prospect

    Science.gov (United States)

    Bahgat, Gawdat

    1999-03-01

    For the last several decades there has been tremendous expansion in the educational facilities in all the six Gulf monarchies (Bahrain, Kuwait, Oman, Qatar, Saudi Arabia, and the United Arab Emirates). The quality of education, however, does not correspond to the needs of Gulf societies. This study examines three of the apparent deficiencies in the educational system in the region: the mismatch between traditional and modern learning, the imbalance between indigenous and expatriate labor forces, and the gap between men and women. The paper concludes that a fundamental change in the quality of education needs to be made in order to overcome these imbalances.

  8. Crustal Deformation in the Southwestern Gulf of Mexico: Underthrusting of the Gulf of Mexico beneath Tehuantepec

    Science.gov (United States)

    Suarez, Gerardo; Aguilar, Sergio

    2016-04-01

    An array of 45 broad band sensors were installed along the Isthmus of Tehuantepec in southeastern. This experiment, called VEOX, was implemented on August 2007 to March 2009. Data were registered continuously during the whole period. In order to search in the seismic records of the data obtained for crustal events in the Isthmus of Tehuantepec, To this purpose, an STA/LTA algorithm was designed to detect earthquakes with S-P times indicating they occurred close the seismic stations, at crustal or upper mantle depths. During the 18 months that the experiment lasted, about 40 crustal earthquakes were recorded in more than three stations, allowing us to determine a hypo central location. All earthquakes occurring at depths greater than 120 km, within the subjected slab, were discarded. The majority of this crustal or upper mantle activity occurred in the northern part of the Isthmus, along the coast of the Gulf of Mexico or just inland from it. No velocity model exists in the area. Therefore, we tested three different velocity models, including one obtained in an adjacent region and based on seismic refraction data. One of these three models rendered the more stable solutions and smaller errors in the hypocentral locations and was used as the local seismic velocity model. In order to improve the quality of the locations, we experimented using a double difference hypocentral algorithm (HYPODD). There was no noticeable improvement in the quality of the hypocenters using this technique. The best located events suggest a southwestern-dipping zone of seismic seismicity, deepening from the Gulf of Mexico towards the interior of the Isthmus of Tehuantepec. The focal mechanisms of the earthquakes indicate the maximum axis of compresion (P axis) is oriented nearly horizontally and in a southwest-northeast direction. These mechanisms are similar to those observed for earthquakes previously studied in the region on the basis of teleseismic data, such as the Mw 6.9, 29 August

  9. Wisconsinan-Holocene seismic stratigraphy of the Keathley Canyon Area and vicinity, northwestern Gulf of Mexico

    Energy Technology Data Exchange (ETDEWEB)

    Lee, Gwang Hoon; Bryant, W.R.; Watkins, J.S. (Texas A and M Univ., College Station (United States))

    1991-03-01

    The lower continental slope of the northwestern Gulf of Mexico is characterized by a hummocky topography with shallow salt masses interspersed by numerous salt-withdrawal basins containing thick Plio-Pleistocene and older sediments. Analysis of over 7500 km of multichannel seismic reflection data from the Keathley Canyon Area and vicinity defined the Wisconsinan-Holocene sequence and its seismic facies. In interbasinal areas and in the southern part of the study area where salt is shallow, the Wisconsinan-Holocene sequence consists mainly of low-amplitude (LA) facies underlain by strong basal-reflection (SBR) facies. The LA facies occasionally show subtle onlaps against SBR facies and grade upward into a draping pattern. Onlapping LA facies are interpreted to be a lowstand systems tract deposited by widespread low-energy turbidity currents. Draping LA facies at the top may consist of hemipelagic or pelagic sediments. The SBR facies are interpreted to consist of condensed sections formed during sea-level rises and highstands. Within basins, moderate-to-high amplitude-continuous (MHC) and hummocky-to-chaotic (HC) facies occur below LA facies. The MHC facies show a pattern of flat-lying or gently dipping reflections that onlap SBR facies. Onlapping MHC facies often grade upward into a conformable pattern and are obscured by transition into LA facies. The MHC facies are interpreted as alternating coarse- and fine-grained turbidites deposited during sea-level falls and/or lowstands. The HC facies occur commonly associated with MHC facies. The HC facies may represent slope fans formed by mass-transport processes or gravity flows during sea-level falls and/or lowstands.

  10. Contributions to the sea level seasonal cycle within the Gulf of Cadiz (Southwestern Iberian Peninsula)

    Science.gov (United States)

    Laiz, Irene; Tejedor, Begoña; Gómez-Enri, Jesús; Aboitiz, Alazne; Villares, Pilar

    2016-07-01

    The spatial distribution of the sea level seasonal cycle within the Gulf of Cadiz (GoC) has been analysed using monthly maps of sea level anomalies from gridded multi-mission altimeter data, along with monthly means of sea level heights from three tide gauge stations. Moreover, the contribution to the sea level seasonal cycle of atmospheric pressure and wind and the steric effect were evaluated using maps of sea level residuals from the VANI2-ERA hindcast, and a combination of satellite Sea Surface Temperature maps with a very high resolution Temperature and Salinity climatology for the region. The atmospheric contribution accounted for 55-58% of the sea level variance offshore, with this percentage diminishing toward the coast, where the effect of wind stress might be underestimated, especially over regions of complex bathymetry. The steric contribution was addressed by considering local, open ocean, basin-wide and continental shelf steric effects. Results obtained highlighted the oceanographic complexity of the GoC at regional scales. In this sense, the open ocean steric contribution explained the largest percentage of atmospheric-corrected sea level variance at the offshore part of the basin (50-67%) and over the eastern shelf (42-48%), suggesting that the sea level seasonal cycle within the eastern shelf is connected to the large scale circulation system. West of Cape Santa Maria, both over the continental shelf and offshore, the best results were obtained with the local steric contribution, suggesting a decoupling of deep and shallow water sea level variations at the seasonal scale in that region.

  11. Plio-Quaternary kinematic development and paleostress pattern of the Edremit Basin, western Turkey

    Science.gov (United States)

    Gürer, Ömer Feyzi; Sangu, Ercan; Özburan, Muzaffer; Gürbüz, Alper; Gürer, Aysan; Sinir, Hasan

    2016-06-01

    The Edremit Basin and Kazdağ High are the most prominent morphological features of the Biga Peninsula in northwest Anatolia. There is still no consensus on the formation of Edremit Basin and debates are on whether the basin evolved through a normal, a right-lateral or a left-lateral strike-slip faulting. In this study, the geometric, structural and kinematic characteristics of the Edremit Basin are investigated to make an analytical approach to this problem. The structural and kinematic features of the faults in the region are described according to field observations. These fault-slip data derived from the fault planes were analyzed to determine the paleostress pattern of faulting in the region. According to the performed analysis, the southern end of the Biga Peninsula is under the influence of the ENE-WSW-trending faults of the region, such as the Yenice-Gönen, the Edremit, the Pazarköy and the Havran-Balıkesir Fault Zones. The right step-over geometry and related extension caused to the development of the Edremit Basin as a transtensional pull-apart basin between the Havran-Balıkesir Fault Zone and the Edremit Fault Zone. Field observations showed that the Plio-Quaternary faults at the Edremit Gulf and adjacent areas are prominently right-lateral strike-slip faults. Our paleostress analyses suggest a dominant NE-SW extension in the study area, as well as NW-SE direction. This pattern indicates the major effects of the North Anatolian Fault System and the component of Aegean Extensional System in the region. However, our kinematic analysis represents the dominant signature of the North Anatolian Fault System in basin bounding faults. The field observations and kinematic findings of this study are also consistent with the regional GPS, paleomagnetic and seismological data. This study concludes that the North Anatolian Fault System is the prominent structure in the current morphotectonic framework of the Edremit Gulf and adjacent areas.

  12. Intracontinental basins and strong earthquakes

    Institute of Scientific and Technical Information of China (English)

    邓起东; 高孟潭; 赵新平; 吴建春

    2004-01-01

    The September 17, 1303 Hongtong M=8 earthquake occurred in Linfen basin of Shanxi down-faulted basin zone. It is the first recorded M=8 earthquake since the Chinese historical seismic records had started and is a great earthquake occurring in the active intracontinental basin. We had held a Meeting of the 700th Anniversary of the 1303 Hongtong M=8 Earthquake in Shanxi and a Symposium on Intracontinental Basins and Strong Earthquakes in Taiyuan City of Shanxi Province on September 17~18, 2003. The articles presented on the symposium discussed the relationships between active intracontinental basins of different properties, developed in different regions, including tensional graben and semi-graben basins in tensile tectonic regions, compression-depression basins and foreland basins in compressive tectonic regions and pull-apart basins in strike-slip tectonic zones, and strong earthquakes in China. In this article we make a brief summary of some problems. The articles published in this special issue are a part of the articles presented on the symposium.

  13. Uranium and other natural radionuclides in the sediments of a Mediterranean fjord-like embayment, Amvrakikos Gulf (Ionian Sea), Greece

    International Nuclear Information System (INIS)

    The distribution of the natural radionuclides (238U, 232Th, 226Ra, 40K) and the artificial 137Cs was studied in sediment cores collected from Amvrakikos Gulf, a seasonal anoxic marine basin, using γ-ray spectrometry. The activity of radionuclides, along with the concentrations of Fe and Mn, were also studied in relation to the total organic carbon and the granulometric fractions of the sediments. The results obtained revealed higher 238U activity concentrations in all the examined sediment samples compared to the world and Greek average values for soil. The high activity values of 238U are attributed, besides the lattice-held fraction, to phosphate fertilizer inputs in the Gulf via major rivers and/or to alteration processes of phosphate ores located mainly in the drainage basin of the river Louros. The elevated activity values of 40K could be attributed to the mineralogical composition of the sediments and to phosphate fertilizers containing potassium. Organic matter seems to be a more efficient sorbent for U than clay minerals and amorphous Fe and Mn-oxyhydroxides. Scanning electron microscopy, together with qualitative analysis of some smectites, reveals the occurrence of U, suggesting a limited absorption of U onto clay minerals. The applied BCR sequential extraction procedure revealed that U was found mainly in the refractory phase or associated with organic matter and to a lesser extent as surface-coating oxides, with the exception of one sediment core which is characterized by high content of fresh marine organic matter and presents high percentage of U in the exchangeable fraction. -- Highlights: ► We study the natural radionuclides and 137Cs in the sediments of Amvrakikos Gulf. ► We examine the fractionation of U and Fe in the sediments. ► The elevated activity of 238U could be attributed to phosphate fertilizers inputs. ► U was found mainly in the refractory phase or associated with organic matter. ► Fe was found associated with the refractory

  14. Gulf of Mexico Climate, Laurentide Ice Sheet History, and Global Sea Level Change During the Last Glacial Cycle

    Science.gov (United States)

    Flower, B. P.; Williams, C.; Brown, E. A.; Hastings, D. W.; Hill, H.; Adams, S.; Hendrix, J.; Martin, E. E.; Biller, N. B.; Goddard, E.

    2011-12-01

    The interactions between low-latitude Atlantic climate and high-latitude ice sheet variability represent an important issue in past abrupt climate change. Specifically, Laurentide Ice Sheet (LIS) meltwater input seems to be decoupled at the millennial scale from Gulf of Mexico sea-surface temperature (SST), as well as Greenland air temperature, during the last glacial cycle. Indeed, comparison to Greenland ice core records indicate significant meltwater input during some North Atlantic cool episodes, including Heinrich Stadials 4, 3, and 1. Here we present published and new Mg/Ca and δ18O data on the planktic foraminifer Globigerinoides ruber from northern Gulf of Mexico sediment cores that provide detailed records of SST, δ18O of seawater (δ18Osw), and inferred salinity for the 48-10 ka interval. Age control for Orca Basin cores MD02-2550 and -2551 is based on AMS 14C dates on G. ruber and documents continuous sedimentation at rates >35 cm/kyr. Significant meltwater input is inferred from δ18Osw data during Antarctic Isotope Maxima (AIM) events and reaches a peak during the Bølling/Allerød, consistent with bipolar warming and a high sensitivity to greenhouse forcing. Furthermore, bulk sediment δ18O data show a brief spike reaching -5.5% ca. 14.5 ka during an interval barren of foraminifera. We speculate that this excursion represents fine carbonate sediment from Canadian Paleozoic marine carbonates, analogous to detrital carbonate in the North Atlantic that has a δ18O value of -5%. Radiogenic isotope data (Nd and Pb) also reach peak values at this interval, indicative of older continental material sourced from Canada vs. younger material from the Mississippi River drainage basin. Inferred major meltwater flow appears to have been associated with meltwater pulse 1a within the Bølling warm interval, consistent with a significant contribution by the LIS to rapid global sea level rise. Overall, the relations between Gulf of Mexico meltwater input, Heinrich

  15. Multiple oscillatory modes of the Argentine Basin. Part II. The spectral origin of the basin modes

    NARCIS (Netherlands)

    Weijer, W.; Vevier, F.; Gille, S.T.; Dijkstra, H.A.

    2007-01-01

    In this paper the spectrum of barotropic basin modes of the Argentine Basin is shown to be connected to the classical Rossby basin modes of a flat-bottom (constant depth), rectangular basin. First, the spectrum of basin modes is calculated for the Argentine Basin, by performing a normal-mode analysi

  16. Earthquake source parameters for the 2010 western Gulf of Aden rifting episode

    Science.gov (United States)

    Shuler, Ashley; Nettles, Meredith

    2012-08-01

    On 2010 November 14, an intense swarm of earthquakes began in the western Gulf of Aden. Within a 48-hr period, 82 earthquakes with magnitudes between 4.5 and 5.5 were reported along an ˜80-km-long segment of the east-west trending Aden Ridge, making this swarm one of the largest ever observed in an extensional oceanic setting. In this study, we calculate centroid-moment-tensor solutions for 110 earthquakes that occurred between 2010 November and 2011 April. Over 80 per cent of the cumulative seismic moment results from earthquakes that occurred within 1 week of the onset of the swarm. We find that this sequence has a b-value of ˜1.6 and is dominated by normal-faulting earthquakes that, early in the swarm, migrate westwards with time. These earthquakes are located in rhombic basins along a section of the ridge that was previously characterized by low levels of seismicity and a lack of recent volcanism on the seafloor. Body-wave modelling demonstrates that the events occur in the top 2-3 km of the crust. Nodal planes of the normal-faulting earthquakes are consistent with previously mapped faults in the axial valley. A small number of strike-slip earthquakes observed between two basins near 44°E, where the axial valley changes orientation, depth and width, likely indicate the presence of an incipient transform fault and the early stages of ridge-transform segmentation. The direction of extension accommodated by the earthquakes is intermediate between the rift orthogonal and the direction of relative motion between the Arabian and Somalian plates, consistent with the oblique style of rifting occurring along the slow-spreading Aden Ridge. The 2010 swarm shares many characteristics with dyke-induced rifting episodes from both oceanic and continental settings. We conclude that the 2010 swarm represents the seismic component of an undersea magmatic rifting episode along the nascent Aden Ridge, and attribute the large size of the earthquakes to the combined effects of

  17. Holocene climate variability in the North-Western Mediterranean Sea (Gulf of Lions)

    Science.gov (United States)

    Jalali, B.; Sicre, M.-A.; Bassetti, M.-A.; Kallel, N.

    2016-01-01

    Sea surface temperatures (SSTs) and land-derived input time series were generated from the Gulf of Lions inner-shelf sediments (NW Mediterranean Sea) using alkenones and high-molecular-weight odd-carbon numbered n-alkanes (TERR-alkanes), respectively. The SST record depicts three main phases: a warm Early Holocene ( ˜ 18 ± 0.4 °C) followed by a cooling of ˜ 3 °C between 7000 and 1000 BP, and rapid warming from ˜ 1850 AD onwards. Several superimposed multi-decadal to centennial-scale cold events of ˜ 1 °C amplitude were also identified. TERR-alkanes were quantified in the same sedimentary horizons to identify periods of high Rhone River discharge and compare them with regional flood reconstructions. Concentrations show a broad increase from the Early Holocene towards the present with a pronounced minimum around 2500 BP and large fluctuations during the Late Holocene. Comparison with Holocene flood activity reconstructions across the Alps region suggests that sediments of the inner shelf originate mainly from the Upper Rhone River catchment basin and that they are primarily delivered during positive North Atlantic Oscillation (NAO).

  18. Distributions and accumulation rates of polycyclic aromatic hydrocarbons in the northern Gulf of Mexico sediments.

    Science.gov (United States)

    Adhikari, Puspa L; Maiti, Kanchan; Overton, Edward B; Rosenheim, Brad E; Marx, Brian D

    2016-05-01

    Sediment samples collected from shelf, slope and interior basin of the northern Gulf of Mexico during 2011-2013, 1-3 years after the Deepwater Horizon (DWH) oil spill, were utilized to characterize PAH pollution history, in this region. Results indicate that the concentrations of surface ΣPAH43 and their accumulation rates vary between 44 and 160 ng g(-1) and 6-55 ng cm(-2) y(-1), respectively. ΣPAH43 concentration profiles, accumulation rates and Δ(14)C values are significantly altered only for the sediments in the immediate vicinity of the DWH wellhead. This shows that the impact of DWH oil input on deep-sea sediments was generally limited to the area close to the spill site. Further, the PAHs source diagnostic analyses suggest a noticeable change in PAHs composition from higher to lower molecular weight dominance which reflects a change in source of PAHs in the past three years, back to the background composition. Results indicate low to moderate levels of PAH pollution in this region at present, which are unlikely to cause adverse effects on benthic communities. PMID:26895564

  19. Oil in nearshore subtidal sediments of Saudi Arabia from the Gulf War spill

    International Nuclear Information System (INIS)

    Detailed sedimentological and dynamic-process studies of the shallow, subtidal habitats of Dawhats ad Dafi and al Mussallamiyah and the bays at Tanaqib on the Saudi Arabian coast were carried out one year after the Gulf War oil spill. These studies were part of Leg II of the NOAA ship Mt. Mitchell cruise. Satellite imagery and space shuttle photography were used extensively to develop detailed study plans. Work accomplished during the study included deployment of three current meters, a tide gauge, and suspended sediment traps (at seven locations). Bathymetric surveys were conducted along 14 transects, and 197 bottom observation dives were carried out. More than 170 bottom sediment samples were collected for chemical and/or textural analysis. Sediment hydrocarbon screening by HPLC fluorescence was conducted on board to verify and refine the sampling plan. The results to date show no evidence of large-scale sinking of oil as a result of the spill. Subtidal oil, as sparse tar balls, was visually observed by divers at three locations, all of which were associated with the erosion of oiled sand from outer beaches. On-board chemical results showed that subtidal sediments have been contaminated at levels ranging from 20 to 2,000 mg petroleum hydrocarbons/kg, with the highest contamination up in the sheltered, muddy basins. However, the oil initially stranded in the intertidal zone does not appear to be accumulating in the nearshore subtidal region in significant quantities one year later

  20. Extending field life in offshore Gulf of Mexico using 3-D seismic survey

    Energy Technology Data Exchange (ETDEWEB)

    Bulling, T.P.; Olsen, R.S. (ARCO Oil and Gas Co., Houston, TX (USA))

    1990-05-01

    Discovered by ARCO in 1967, the High Island 24L field (lower Miocene) is located in the Texas state waters of the Gulf of Mexico. By 1986, the field had produced 320 billion ft{sup 3} of gas and 3.0 million bbl of oil. An engineering field study completed in 1986 showed the field was declining and would be unprofitable within 3 yr. Study of reservoir maps revealed three basin problems: volumetric reserve calculations were less than reserves produced, hydrocarbon-water contacts were inconsistent between wells thought to be in communication, and ultimate recoveries could not be accurately calculated. Attempts to remap the field with the existing two-dimensional seismic data base and well data proved unsuccessful. In 1986, a three-dimensional seismic survey was acquired in an effort to evaluate the true present worth and potential of the field. Remapping of 30 reservoir horizons began in 1987. The integration of detailed well log correlations tied to the dense grid of quality three dimensional seismic data improved the reservoir maps. These maps helped resolve engineering problems by defining the configuration of the reservoirs more accurately. Reservoir maps now closely match volumetrics, fluid contacts within reservoir units are consistent, and a better definition of extension well opportunities exists. The authors study resulted in six additional wells. These wells along with engineering modifications and operations cost containment resulted in the extension of the economic life of the High Island 24-L field by at least 8 yr.

  1. Holocene climate variability in the North-Western Mediterranean Sea (Gulf of Lions

    Directory of Open Access Journals (Sweden)

    B. Jalali

    2015-07-01

    Full Text Available Sea surface temperatures (SSTs and land-derived input time series were generated from the Gulf of Lions inner-shelf sediments (NW Mediterranean Sea using alkenones and high-molecular-weight odd-carbon numbered n-alkanes (TERR-alkanes, respectively. The SST record depicts three main phases: a warm Early Holocene (∼ 18 ± 0.4 °C followed by a cooling of ∼ 3 °C (from 7000 to 1000 BP and rapid warming from ∼ 1850 AD onwards. Several superimposed multi-decadal cooling events of ∼ 1 °C amplitude were also identified. TERR-alkanes were also quantified to identify periods of high river discharge in relation with flood events of the Rhone River and precipitations. Their concentrations show a broad increase from the early Holocene towards present with a pronounced minimum around 2500 BP and large fluctuations during the second part of the Holocene. Comparison with Holocene flood activity reconstructions across the Alps region suggests that sediments of the inner shelf originate mainly from the Upper Rhone River catchment basin and that they are primarily delivered during positive NAO.

  2. A Holocene pollen and diatom record from Vanderlin Island, Gulf of Carpentaria, lowland tropical Australia

    Science.gov (United States)

    Prebble, Matiu; Sim, Robin; Finn, Jan; Fink, David

    2005-11-01

    Sedimentary, palynological and diatom data from a dunefield lake deposit in the interior of Vanderlin Island in the Gulf of Carpentaria are presented. Prior to the formation of present perennial lake conditions, the intensified Australian monsoon associated with the early Holocene marine transgression allowed Cyperaceae sedges to colonise the alluvial margins of an expansive salt flat surrounded by an open Eucalyptus woodland. As sea level stabilised between 7500 and 4500 cal yr B.P. coastal dunes ceased to develop allowing dense Melaleuca forest to establish in a Restionaceae swamp. Dune-sand input into the swamp was diminished further as the increasingly dense vegetation prevented fluvial and aeolian transported sand arriving from coastal sources. This same process impounded the drainage basin allowing a perennial lake to form between 5500 and 4000 cal yr B.P. Myriophyllum and other aquatic taxa colonised the lake periphery under the most extensive woodland recorded for the Holocene. The palynological data support an effective precipitation model proposed for northern Australia that suggests more variable conditions in the late Holocene. A more precise measure of effective precipitation change is provided by diatom-based inferences that indicate few changes in lake hydrology. Such interpretations are explained in terms of palynological sensitivity to adjustments in local fire regimes where regional precipitation change may only be recorded indirectly through fire promoting mechanisms, including intensified ENSO periodicity and human impact.

  3. Apollo Basin, Moon: Estimation of Impact Conditions

    Science.gov (United States)

    Echaurren, J. C.

    2015-07-01

    The Apollo Basin is a, pre-Nectarian, multi-ring basin located within the large South Pole-Aitken Basin (SPA). Multispectral data from both Galileo and Clementine showed that the composition of materials in Apollo is distinct…

  4. Attributes for MRB_E2RF1 Catchments in Selected Major River Basins: Population Density, 2000

    Science.gov (United States)

    Wieczorek, Michael E.; LaMotte, Andrew E.

    2010-01-01

    This data set represents the average population density, in number of people per square kilometer multiplied by 10 for the year 2000, compiled for every MRB_E2RF1 catchment of selected Major River Basins (MRBs, Crawford and others, 2006). The source data set is the 2000 Population Density by Block Group for the Conterminous United States (Hitt, 2003). The MRB_E2RF1 catchments are based on a modified version of the U.S. Environmental Protection Agency's (USEPA) RF1_2 and include enhancements to support national and regional-scale surface-water quality modeling (Nolan and others, 2002; Brakebill and others, 2011). Data were compiled for every MRB_E2RF1 catchment for the conterminous United States covering covering New England and Mid-Atlantic (MRB1), South Atlantic-Gulf and Tennessee (MRB2), the Great Lakes, Ohio, Upper Mississippi, and Souris-Red-Rainy (MRB3), the Missouri (MRB4), the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf (MRB5), the Rio Grande, Colorado, and the Great basin (MRB6), the Pacific Northwest (MRB7) river basins, and California (MRB8).

  5. 50 CFR Appendix B to Part 622 - Gulf Areas

    Science.gov (United States)

    2010-10-01

    ..., DEPARTMENT OF COMMERCE FISHERIES OF THE CARIBBEAN, GULF, AND SOUTH ATLANTIC Pt. 622, App. B Appendix B to... Florida/Alabama border 29°34.5′ 87°38.0′ 16Off Mobile Bay 29°41.0′ 88°00.0′ 17South of...

  6. U-Th series nuclides in the Gulf of Mexico

    International Nuclear Information System (INIS)

    A study of U and Th series nuclides is being conducted on sediments from the Gulf of Mexico. Uranium concentrations as a function of depth have been determined, as well as changes in the 234U/238U activity ratio. The geochemical behavior of uranium in shelf sediments is discussed

  7. Binational collaboration to study Gulf of Mexico's harmful algae

    Science.gov (United States)

    Soto, Inia; Hu, Chuanmin; Steidinger, Karen; Muller-Karger, Frank; Cannizzaro, Jennifer; Wolny, Jennifer; Cerdeira-Estrada, Sergio; Santamaria-del-Angel, Eduardo; Tafoya-del-Angel, Fausto; Alvarez-Torres, Porfirio; Herrera Silveira, Jorge; Allen, Jeanne

    2012-01-01

    Blooms of the toxic marine dinoflagellate Karenia brevis cause massive fish kills and other public health and economic problems in coastal waters throughout the Gulf of Mexico [Steidinger, 2009]. These harmful algal blooms (HABs) are a gulf-wide problem that require a synoptic observing system for better serving decision-making needs. The major nutrient sources that initiate and maintain these HABs and the possible connectivity of blooms in different locations are important questions being addressed through new collaborations between Mexican and U.S. researchers and government institutions. These efforts were originally organized under the U.S./Mexico binational partnership for the HABs Observing System (HABSOS), led by the U.S. Environmental Protection Agency's Gulf of Mexico Program (EPAGMP) and several agencies in Veracruz, Mexico, since 2006. In 2010 these efforts were expanded to include other Mexican states and institutions with the integrated assessment and management of the Gulf of Mexico Large Marine Ecosystem (GoMLME) program sponsored by the Global Environment Facility (GEF), the United Nations Industrial Development Organization (UNIDO), the Secretaría de Medio Ambiente y Recursos Naturales (SEMARNAT), and the National Oceanic and Atmospheric Administration (NOAA).

  8. Good Order at Sea in the Gulf of Guinea

    DEFF Research Database (Denmark)

    Jacobsen, Katja Lindskov; Nordby, Johannes

    2015-01-01

    In this chapter, we first outline the maritime security situation in the Gulf of Guinea region at present. It is examined in the context of Good Order at Sea. Second, we describe the most recent maritime security initiative launched during the Yaoundé Summit in 2013. During the summit, West and C...

  9. 78 FR 54801 - Gulf Coast Restoration Trust Fund

    Science.gov (United States)

    2013-09-06

    ... Sustainability, Tourist Opportunities, and Revived Economies of the Gulf Coast States Act of 2012 (RESTORE Act... attributable to Trust Fund management? III. Regulatory Planning and Review (Executive Orders 12866 and 13563... part 34 to read as follows: PART 34--RESOURCES AND ECOSYSTEMS SUSTAINABILITY, TOURIST...

  10. Marine and Estuarine Ecology. Man and the Gulf of Mexico.

    Science.gov (United States)

    Irby, Bobby N.; And Others

    "Man and the Gulf of Mexico (MGM)" is a marine science curriculum developed to meet the marine science needs of tenth through twelfth grade students in Mississippi and Alabama schools. This MGM unit, which focuses on marine and estuarine ecology, is divided into six sections. The first section contains unit objectives, discussions of the estuarine…

  11. Wind farm planning at the Gulf of Suez

    Energy Technology Data Exchange (ETDEWEB)

    Clausen, N.E.; Mortensen, N.G.; Hansen, J.C. [Risoe National Lab., Wind Energy Dept., Roskilde (Denmark); Clausager, I. [Hedeselskabet A/S, Viborg (Denmark); Pagh Jensen, F. [National Environmental Res., Copenhagen (Denmark); Georgy, L.; Said, U.S. [New and Renewable Energy Authority, Egypt, (Egypt)

    2004-11-01

    The Wind Atlas for Egypt project is an element in a national effort to provide the best possible basis for planning of future environmentally sustainable development and utilization of wind energy resources and technology in Egypt. The present report compiles the data, information and recommendations available for planning of wind farm projects in the Gulf of Suez. (au)

  12. Wind Simulations for the Gulf of Suez with KAMM

    DEFF Research Database (Denmark)

    Frank, Helmut Paul

    In order to get a better overview of the spatial distribution of the wind resource in the Gulf of Suez, numerical simulations to determine the wind climate have been carried out with the Karlsruhe Atmospheric Mesoscale Model KAMM. The method and the results are described here. The simulations of...

  13. Toxiological Considerations in the Gulf of Mexico Oil Spill

    Science.gov (United States)

    The Deep Water Horizon oil rig exploded on April 20, 2010, resulting in an ongoing release of light sweet petroleum crude oil and methane into Gulf of Mexico waters. The release from the deepwater wellhead 41 miles from Louisiana is at approximately 1 mile depth, and flow rates e...

  14. "Going Mobile" in Business Communication at an Arabian Gulf University

    Science.gov (United States)

    Rapanta, Chrysi; Nickerson, Catherine; Goby, Valerie Priscilla

    2014-01-01

    In this article, we describe a project in which undergraduate business seniors at a university in the Arabian Gulf created or evaluated the chapters of an iBook as part of their final course in business communication. Students were surveyed throughout the project, and they also participated in a focus group discussion at the end. The aim was to…

  15. Effects of the Gulf Oil Spill in Escambia County, Florida

    Science.gov (United States)

    Killingsworth, Kelcey Ray

    2012-01-01

    The purpose of this study was to assess the impact of the British Petroleum Gulf Oil Spill on resource change, psychological stress, and resilience for business owners, residents, and workers in Escambia County, Florida. This study was based on Hobfoll's (1988, 1989) Conservation of Resources theory. All business owners, residents, and…

  16. NASA DEVELOP Students Rev Up Response to Gulf Oil Spill

    Science.gov (United States)

    Jones, Jason B.; Childs, Lauren M.

    2010-01-01

    After the April 20th explosion aboard the Deepwater Horizon drilling rig in the Gulf of Mexico, the world witnessed one of the worst oil spill catastrophes in global history. In an effort to mitigate the disaster, the U.S. government moved quickly to establish a unified command for responding to the spill. Some of the command's most immediate needs were to track the movement of the surface oil slick, establish a baseline measurement of pre-oil coastal ecosystem conditions, and assess potential air quality and water hazards related to the spill. To help address these needs and assist the Federal response to the disaster, NASA deployed several of its airborne and satellite research sensors to collect an unprecedented amount of remotely-sensed data over the Gulf of Mexico region. Although some of these data were shared with the public via the media, much of the NASA data on the disaster was not well known to the Gulf Coast community. The need existed to inform the general public about these datasets and help improve understanding about how NASA's science research was contributing to oil spill response and recovery. With its extensive experience conducting community-oriented remote sensing projects and close ties to organizations around Gulf of Mexico, the NASA DEVELOP National Program stood in a unique position to meet this need.

  17. 76 FR 65321 - Gulf War Veterans' Illnesses Task Force

    Science.gov (United States)

    2011-10-20

    ... download the Gulf War Veterans' Illnesses Task Force Draft Report for Public Comment at http://www.va.gov... submission of public comments through http://www.regulations.gov ; written comments may be submitted through... period, through the Federal Docket Management System (FDMS) at http://www.regulations.gov . You can...

  18. 77 FR 18307 - Gulf War Veterans' Illnesses Task Force Report

    Science.gov (United States)

    2012-03-27

    ... Veterans' Illnesses Task Force Report is available on the VA Web site at: http://www.va.gov/opa... published the report in the Federal Register (76 FR 65321) and posted it on a social media Web site created...: Notice. SUMMARY: The Secretary Department of Veterans Affairs (VA) established the Gulf War...

  19. 78 FR 28292 - Gulf War Veterans' Illnesses Task Force

    Science.gov (United States)

    2013-05-14

    .... ADDRESSES: Although VA prefers electronic submission of public comments through http://www.regulations.gov... Report for Public Comment at http://www.va.gov/opa/publications/Draft_2012_GWVI-TF_Report.pdf . Please... (FDMS) at http://www.regulations.gov . You can also submit ideas on improving VA services to Gulf...

  20. SOLUTION MINING IN SALT DOMES OF THE GULF COAST EMBAYMENT

    Energy Technology Data Exchange (ETDEWEB)

    Griswold, G. B.

    1981-02-01

    Following a description of salt resources in the salt domes of the gulf coast embayment, mining, particularly solution mining, is described. A scenario is constructed which could lead to release of radioactive waste stored in a salt dome via inadvertent solution mining and the consequences of this scenario are analyzed.

  1. Water use and quality of fresh surface-water resources in the Barataria-Terrebonne Basins, Louisiana

    Science.gov (United States)

    Johnson-Thibaut, Penny M.; Demcheck, Dennis K.; Swarzenski, Christopher M.; Ensminger, Paul A.

    1998-01-01

    Approximately 170 Mgal/d (million gallons per day) of ground- and surface-water was withdrawn from the Barataria-Terrebonne Basins in 1995. Of this amount, surface water accounted for 64 percent ( 110 MgaVd) of the total withdrawal rates in the basins. The largest surface-water withdrawal rates were from Bayou Lafourche ( 40 Mgal/d), Bayou Boeuf ( 14 MgaVd), and the Gulf Intracoastal Waterway (4.2 Mgal/d). The largest ground-water withdrawal rates were from the Mississippi River alluvial aquifer (29 Mgal/d), the Gonzales-New Orleans aquifer (9.5 Mgal/d), and the Norco aquifer (3.6 MgaVd). The amounts of water withdrawn in the basins in 1995 differed by category of use. Public water suppliers within the basins withdrew 41 Mgal/d of water. The five largest public water suppliers in the basins withdrew 30 Mgal/d of surface water: Terrebonne Waterworks District 1 withdrew the largest amount, almost 15 MgaVd. Industrial facilities withdrew 88 Mgal/d, fossil-fuel plants withdrew 4.7 MgaVd, and commercial facilities withdrew 0.67 MgaVd. Aggregate water-withdrawal rates, compiled by parish for aquaculture (37 Mgal/d), livestock (0.56 Mgal/d), rural domestic (0.44 MgaVd), and irrigation uses (0.54 MgaVd), totaled about 38 MgaVd in the basins. Ninety-five percent of aquaculture withdrawal rates, primarily for crawfish and alligator farming, were from surface-water sources. >br> Total water-withdrawal rates increased 221 percent from 1960–95. Surface-water withdrawal rates have increased by 310 percent, and ground-water withdrawal rates have increased by 133 percent. The projection for the total water-withdrawal rates in 2020 is 220 MgaVd, an increase of 30 percent from 1995. Surface-water withdrawal rates would account for 59 percent of the total, or 130 Mgal/d. Surface-water withdrawal rates are projected to increase by 20 percent from 1995 to 2020. Analysis of water-quality data from the Mississippi River indicates that the main threats to surface water resources are

  2. Advanced Chemistry Basins Model

    Energy Technology Data Exchange (ETDEWEB)

    Blanco, Mario; Cathles, Lawrence; Manhardt, Paul; Meulbroek, Peter; Tang, Yongchun

    2003-02-13

    The objective of this project is to: (1) Develop a database of additional and better maturity indicators for paleo-heat flow calibration; (2) Develop maturation models capable of predicting the chemical composition of hydrocarbons produced by a specific kerogen as a function of maturity, heating rate, etc.; assemble a compositional kinetic database of representative kerogens; (3) Develop a 4 phase equation of state-flash model that can define the physical properties (viscosity, density, etc.) of the products of kerogen maturation, and phase transitions that occur along secondary migration pathways; (4) Build a conventional basin model and incorporate new maturity indicators and data bases in a user-friendly way; (5) Develop an algorithm which combines the volume change and viscosities of the compositional maturation model to predict the chemistry of the hydrocarbons that will be expelled from the kerogen to the secondary migration pathways; (6) Develop an algorithm that predicts the flow of hydrocarbons along secondary migration pathways, accounts for mixing of miscible hydrocarbon components along the pathway, and calculates the phase fractionation that will occur as the hydrocarbons move upward down the geothermal and fluid pressure gradients in the basin; and (7) Integrate the above components into a functional model implemented on a PC or low cost workstation.

  3. Atlantic Basin refining profitability

    International Nuclear Information System (INIS)

    A review of the profitability margins of oil refining in the Atlantic Basin was presented. Petroleum refiners face the continuous challenge of balancing supply with demand. It would appear that the profitability margins in the Atlantic Basin will increase significantly in the near future because of shrinking supply surpluses. Refinery capacity utilization has reached higher levels than ever before. The American Petroleum Institute reported that in August 1997, U.S. refineries used 99 per cent of their capacity for several weeks in a row. U.S. gasoline inventories have also declined as the industry has focused on reducing capital costs. This is further evidence that supply and demand are tightly balanced. Some of the reasons for tightening supplies were reviewed. It was predicted that U.S. gasoline demand will continue to grow in the near future. Gasoline demand has not declined as expected because new vehicles are not any more fuel efficient today than they were a decade ago. Although federally-mandated fuel efficiency standards were designed to lower gasoline consumption, they may actually have prevented consumption from falling. Atlantic margins were predicted to continue moving up because of the supply and demand evidence: high capacity utilization rates, low operating inventories, limited capacity addition resulting from lower capital spending, continued U.S. gasoline demand growth, and steady total oil demand growth. 11 figs

  4. Petroleum service projects in the Gulf of Guinea

    Science.gov (United States)

    Ken-Worgu, Kenneth Chukwumeka

    2011-07-01

    The goal of this record of study is to examine the major facets involved in managing several petroleum service projects located in three different countries in the Gulf of Guinea simultaneously, while effectively engaging in business development activities for the Oil and Industrial Services Group (OIS). This work also furnishes adequate background on related subject matters to enable understanding of the projects presented. The petroleum services sector is the back bone of the oil and gas industry. Services companies are vital to the success of all petroleum and energy producers in the USA, the Gulf of Guinea and the world. There is a need and demand for these service companies because they play various roles such as logistics, drilling, construction, dredging, pipe laying, procurement, food supply, human resource supply, etc. The Gulf of Guinea comprises of countries from west and central Africa. This project was limited to Nigeria, Equatorial Guinea and Cameroon. This area holds the largest petroleum reserves in Africa and plays a vital role in the global supply of petroleum. The Oil and Industrial Services Group (OIS), plans to establish herself as one of the leading petroleum service companies in this gulf. To manage this expansion, I have taken the role of Gulf of Guinea manager to apply my background as a petroleum engineer as well as my business skills to build a successful division of the company. This work provides a record of study of the management of services, projects and contracts carried out by the OIS group in the gulf of Guinea. The following are the specific projects in the Gulf of Guinea that I participated in: Managing delivering, maintenance and marketing of offshore vessels, Offshore pipe laying project, Integrated pipeline maintenance project, Development a petroleum technical training facilities, Agbami pipe insulation project, Engineering lift project and Capital budgeting analysis for potential investments. The details of the specific

  5. Structural model of the Trieste Gulf: A proposal

    Science.gov (United States)

    Carulli, Giovanni Battista

    2011-03-01

    The onshore geology of the Trieste Gulf is well known in Italian reliefs, as well as in Slovenian and Croatian ones (Istria peninsula). In the northeastern and southern part carbonate platforms outcrop mainly in shelf facies of the Cretaceous to the Paleogene ages and are covered by Eocene flysch deposits. In the northern part the Gulf is closed by the coastal line of the Friuli plain composed mainly of glacio-fluvial deposits of Quaternary age. From a structural point of view, overthrusts set in a typical Dinaric NW-SE direction dominate and where one can identifiy many tectonic units with a SW vergence, tending to overlap the Mesozoic-Paleogene carbonate units which lie over the Eocene terrigenous ones. In this general picture, some sub-vertical faults with an anti-Dinaric NE-SW orientation and a strike-slip activity, cut the previous overthrusts. On the other hand the offshore geological knowledge of the Gulf is scarce due also to the absence, in the inner part of the Gulf, of exploration wells. Only recent studies on some tectonic structures of the Trieste Gulf revealed by geophysical explorations made a few years ago, have suggested making a hypothesis on its formation that has never been studied before. The model proposed here starts from the hypothesis that all tectonic lines that come from the Italian, Slovene and Croatian coastline, continue offshore. This is validated by highlighting all the geometries and morphologic anomalies obtained by analyzing various documents that regard the buried subsoil and obtained through geophysical prospections. With this idea, the maps showing the isobaths of the top of the limestones, the depth and structures of the top of the flysch, the isobaths of the base of the Quaternary deposits and the morphology of the actual sea bed were compared. All these documents present many morphological elements, found repeatedly on maps with different finalities but which appear coherent with the general picture of the structural outcrop

  6. Interaction between salt flow and sedimentation in the Gulf of Mexico

    Science.gov (United States)

    Brun, Jean-Pierre; Fort, Xavier

    2013-04-01

    The northern Gulf of Mexico (GoM) is likely the most spectacular salt margin worlwide. Whereas salt was deposited in late Jurassic, a massive extrusion of allochthonous salt bodies occurred during the Cenozoic, as much as 8 km thick in some places, on top of which Neogene minibasins are deposited. The presence of minibasins, sometimes very deep, have strengthened the impression that salt tectonics was mainly driven by differential sedimentary loading. However, the kinematic analysis of relative displacements between minibasins using digital bathymetry of the slope area over a 450x250 km area indicates a consistent SW direction of salt flow at slope scale. Simultaneously, the shelf break has migrated over approximately 400 km since the Cretaceous with a sudden acceleration in middle-Miocene. In a salt basin, a shelf can form and stabilize only if the salt layer underlying the sediments stops flowing or is flowing at a very low rate. Therefore, at a given moment of basin evolution, a shelf break contour represents the boundary between the seaward part of the basin still deforming above the flowing salt and the landward part where salt has stopped flowing and where previous structures are sealed by sediments being deposited. If sedimentation is oblique to the direction of salt flow, transfer zones develop parallel to the salt flow during shelf break migration. In the northern GoM, where sedimentary progradation is dominantly directed to the south, transfer zones trend in a mean NE-SW direction indicating a SW directed salt direction, like in the slope, with a mean obliquity of around 55° between the directions of sediment progradation and salt flow. Structural analysis of 2D-3D seismics shows that massive salt extrusion and acceleration of shelf break migration are coeval with the failure of the salt basin front in middle-Miocene, allowing a frontal salt nappe to flow over more than 100 km. To test this kinematic interpretation, we carried out laboratory experiments

  7. Intrinsic and forced interannual variability of the Gulf of Alaska mesoscale circulation

    Science.gov (United States)

    Combes, Vincent; Di Lorenzo, Emanuele

    2007-10-01

    The response of the Gulf of Alaska (GOA) circulation to large-scale North Pacific climate variability is explored using three high resolution (15 km) regional ocean model ensembles over the period 1950-2004. On interannual and decadal timescales the mean circulation is strongly modulated by changes in the large scale climate forcing associated with PDO and ENSO. Intensification of the model gyre scale circulation occurs after the 1976-1977 climate shift, as well as during 1965-1970 and 1993-1995. From the model dynamical budgets we find that when the GOA experiences stronger southeasterly winds, typical during the positive phase of the PDO and ENSO, there is net large-scale Ekman convergence in the central and eastern coastal boundary. The geostrophic adjustment to higher sea surface height (SSH) and lower isopycnals lead to stronger cyclonic gyre scale circulation. The opposite situation occurs during stronger northwesterly winds (negative phase of the PDO). Along the eastern side of the GOA basin, interannual changes in the surface winds also modulate the seasonal development of high amplitude anticyclonic eddies (e.g. Haïda and Sitka eddies). Large interannual eddy events during winter-spring, are phase-locked with the seasonal cycle. The initial eddy dynamics are consistent with a quasi-linear Rossby wave response to positive SSH anomalies forced by stronger downwelling favorable winds (e.g. southwesterly during El Niño). However, because of the fast growth rate of baroclinic instability and the geographical focusing associated with the coastal geometry, most of the perturbation energy in the Rossby wave is locally trapped until converted into large scale nonlinear coherent eddies. Coastally trapped waves of tropical origin may also contribute to positive SSH anomalies that lead to higher amplitude eddies. However, their presence does not appear essential. The model ensembles, which do not include the effects of equatorial coastally trapped waves, capture the

  8. Psychiatric consequences of WTC collapse and the Gulf War

    Directory of Open Access Journals (Sweden)

    Ajai R. Singh

    2004-05-01

    Full Text Available Along with political, economic, ethical, rehabilitative and military dimensions, psychopathological sequelae of war and terrorism also deserve our attention. The terrorist attack on the World Trade Centre ( W.T.C. in 2001 and the Gulf War of 1990-91 gave rise to a number of psychiatric disturbances in the population, both adult and children, mainly in the form of Post-traumatic Stress disorder (PTSD. Nearly 75,000 people suffered psychological problems in South Manhattan alone due to that one terrorist attack on the WTC in New York and the Pentagon in Washington. In Gulf War I, morethat 1,00,000 US veterans reported a number of health problems on returning from war, whose claims the concerned government has denied in more than 90% cases. Extensive and comprehensive neurological damage to the brain of Gulf War I veterans has been reported by one study, as has damage to the basal ganglia in another, and Amyotrophic Lateral Sclerosis (ALS in a third,possibly due to genetic mutations induced by exposure to biological and chemical agents, fumes from burning oil wells, landfills,mustard or other nerve gases. The recent Gulf War will no doubt give rise its own crop of PTSD and related disorders. In a cost-benefitanalysis of the post Gulf War II scenario, the psychopathological effects of war and terrorism should become part of the social audit any civilized society engages in. Enlightened public opinion must become aware of the wider ramifications of war and terrorism so that appropriate action plans can be worked out.

  9. Satellite-measured seasonal and inter-annual chlorophyll variability in the Northeast Pacific and Coastal Gulf of Alaska

    Science.gov (United States)

    Brickley, Peter J.; Thomas, Andrew C.

    2004-01-01

    Four years (September 1997-August 2001) of SeaWiFS ocean-color satellite data are used to present the first synoptic quantification of chlorophyll variability on seasonal and interannual timescales over the Northeast Pacific and Coastal Gulf of Alaska. Low light levels and/or cloud during November-January prevent examination of winter patterns. The climatological seasonal patterns show shelf-intensified chlorophyll (by a factor of 3 or more) around the entire basin, extending up to 300 m beyond the shelfbreak along the eastern margin and south of Kodiak Island, with peaks in May and again but weaker in August-September. Over the central basin, concentrations are minimum in February (GOA. Cross-shelf chlorophyll variability (0-400 km offshore) at three locations contrasts strong seasonality and spring bloom development offshore, over the shelf break, in the northern GOA (off Seward) with weaker seasonality over the shelf off the Queen Charlotte Islands. The shelf between Prince William Sound and Kodiak Island consistently develops a spring along-shelf gradient in chlorophyll, maximum over the western end of the shelf. Comparisons to wind and surface temperature anomalies suggest that interannual differences in the strength of the spring bloom are more strongly related to wind forcing the previous winter than temperature anomalies associated with the 1997/98 El Nino.

  10. 76 FR 50181 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2011-08-12

    ... train participating charter boat operators to recognize abnormalities in reef fish and to use..., and South Atlantic; Reef Fish Fishery of the Gulf of Mexico; Exempted Fishing Permit AGENCY: National... Louisiana, is intended to more closely monitor populations of red snapper and other reef fish to...

  11. 77 FR 56168 - Reef Fish Fishery of the Gulf of Mexico; Gulf of Mexico Individual Fishing Quota Programs

    Science.gov (United States)

    2012-09-12

    ... fish fishery (71 FR 67447, November 22, 2006). Amendment 29 to the FMP established an IFQ program for the commercial grouper and tilefish components of the Gulf reef fish fishery (74 FR 44732, August 31... Amendment 26 to the FMP (71 FR 67447, November 22, 2006) and Amendment 29 to the FMP (74 FR 44732, August...

  12. 75 FR 74656 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2010-12-01

    ... value is used as a monetary estimate of the opportunity cost of time on a per hour basis. Thus, the annual opportunity cost per vessel resulting from this requirement is estimated to be approximately $85. For the 951 vessels with valid or renewable commercial Gulf reef fish permits, the annual...

  13. 78 FR 19649 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2013-04-02

    ... strategy for the headboat segment of the recreational fishing sector within the Gulf reef fish fishery... evaluate the efficacy of an allocation-based management strategy, which if proven successful, could... of customers), trip and season-level variable revenues and costs (e.g., trip pricing, gear, bait,...

  14. 77 FR 21955 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2012-04-12

    .... The final rule for Amendment 5 to the FMP for the Shrimp Fishery of the Gulf of Mexico (56 FR 22827... still overfished and under a rebuilding plan through 2032. The next SEDAR benchmark stock assessment... regulatory action. Although the regulatory process required to reopen the season could, in theory,...

  15. 77 FR 75568 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2012-12-21

    ... quotas for red snapper in 2013 at the 2012 level. The intent of this action is to help achieve optimum yield (OY) for the Gulf red snapper resource without increasing the risk of red snapper experiencing...-Stevens Act). On May 30, 2012, NMFS published a final rule (77 FR 31734), that in part, set the...

  16. 78 FR 20292 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2013-04-04

    ... individual states (78 FR 17882, March 25, 2013). The closure dates off each Gulf state would be based on the... red snapper experiencing overfishing. DATES: Written comments must be received on or before April 19... overfishing had ended for the red snapper stock, and that the acceptable biological catch (ABC) may...

  17. 76 FR 13122 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2011-03-10

    ... market greater amberjack as a trophy fish during the months their preferred target species of red snapper...: The comment period for the proposed rule that published on January 24, 2011 (76 FR 4084), and closed... regulatory flexibility analysis (IRFA), and a regulatory impact review, may be obtained from the Gulf...

  18. 75 FR 58335 - Fisheries of the Caribbean, Gulf of Mexico, and South Atlantic; Reef Fish Fishery of the Gulf of...

    Science.gov (United States)

    2010-09-24

    ... red snapper season after September 30, and requested public comment (75 FR 49883). The rationale for... analysis (FRFA), and the regulatory impact review for this rule may be obtained from the Southeast Regional... tourism industries of Gulf coastal communities. The timing and duration of a re-opening will not...

  19. Characterisation of coastal counter-currents on the inner shelf of the Gulf of Cadiz

    Science.gov (United States)

    Garel, E.; Laiz, I.; Drago, T.; Relvas, P.

    2016-03-01

    At the Gulf of Cadiz (GoC), poleward currents leaning along the coast alternate with coastal upwelling jets of opposite direction. Here the patterns of these coastal countercurrents (CCCs) are derived from ADCP data collected during 7 deployments at a single location on the inner shelf. The multiyear (2008-2014) time-series, constituting ~ 18 months of hourly records, are further analysed together with wind data from several sources representing local and basin-scale conditions. During one deployment, temperature sensors were also installed near the mooring site to examine the vertical thermal stratification associated with periods of poleward flow. These observations indicate that the coastal circulation is mainly alongshore and barotropic. However, a baroclinic flow is often observed shortly at the time of flow inversion to poleward. CCCs develop all year-round and exclusively control the occurrence of warm coastal water during the upwelling season. On average, one poleward flow lasting 3 days was observed every week, corresponding to CCCs during ~ 40% of the time without seasonal variability. Thus, the studied region is distinct from typical upwelling systems where equatorward coastal upwelling jets largely predominate. CCCs often start to develop near the bed and are frequently associated with 2-layer cross-shore flows characteristic of downwelling conditions (offshore near the bed). In general, the action of alongshore wind stress alone does not justify the development of CCCs. The coastal circulation is best correlated and shows the highest coherence with south-eastward wind in the basin that proceeds from the rotation of southward wind at the West coast of Portugal, hence suggesting a dominant control of large-scale wind conditions. In agreement, wavelet analyses indicate that CCCs are best correlated with alongshore wind occurring in a band period characteristic of the upwelling system (8-32 days). Furthermore, in the absence of wind coastal currents tend

  20. Basin Dynamics and Sedimentary Infilling of Miocene Sandstone Reservoir Systems In Eastern Tunisian African Margin

    Science.gov (United States)

    Bédir, Mourad; Khomsi, Sami

    2015-04-01

    Most of hydrocarbon accumulations and aquifers within the Cap Bon, Gulf of Hammamet and Sahel basins in eastern tunisian foreland are reservoired within the Upper Miocene Birsa and Saouaf sandstones and shales Formations. In the gulf of Hammamet, these sandstones constitutes oil and gas fields and are exploited on anticline highs and described as varying from shoreface to shallow marine and typically exhibit excellent reservoir quality of 30% to 35% porosity and good permeability from 500 to 1100 md. In addition, the fracturing of faults enhanced the reservoir quality potential. In contrary, the same hydrocarbon reservoirs are important hydrogeologic ones in the Cap Bon and Sahel basins with huge amount of hundred millions of cubic meters of water only partially exploited. Integrated wire line logging correlations, seismic sequence stratigraphic, tectonics and outcrop geologic analogue studies had permitted to highlight the basin structuring and sedimentary environments of sequence deposits infilling of the reservoir distribution between high platforms to subsiding graben and syncline basins bounded by deep-seated transtensive and transpressive flower faults. Seven third order sequence deposits limited by downlap prograding and onlap/toplap aggrading/retrograding system tracts extend along the eastern margin around the three basins by facies and thickness variances. System tracts exhibit around high horst and graben a channelized and levee infillings extending from 100 meters to more than a kilometer of width. They present a stacked single story and multistory channels types showing space lateral and vertical migrations along NE-SW, E-W and N-S directions. Paleogeographic depositional reservoir fair maps distribution highlight deltaic horst domain with floodplain and incised valley of fluvial amalgamed and braided sandstones distributary channels that occupy the high folded horsts. Whereas folded horst-graben and syncline borders domain of Shelf prodelta are

  1. Pre-Messinian (Sub-Salt Source-Rock Potential on Back-Stop Basins of the Hellenic Trench System (Messara Basin, Central Crete, Greece

    Directory of Open Access Journals (Sweden)

    Maravelis A.

    2016-01-01

    Full Text Available The Greek part of the Mediterranean Ridge suggests, in terms of its hydrocarbon potential, further frontier exploration. The geological similarities between its prolific portions, within the Cyprus and Egyptian Exclusive Economic Zones, indicate possible recoverable natural gas reserves in its Greek portion. Nevertheless it lacks of systematic frontier exploration although direct petroleum indicators occur. Active mud volcanoes on the Mediterranean Ridge, still emitting concurrently gas and gas hydrates, have not been yet assessed even though are strongly related to hydrocarbon occurrence worldwide (Caspian Sea, Gulf of Mexico, Western African Basin, Trinidad-Tobago, the Nile Cone. For this reason, the source rock potential of the Late Miocene lacustrine deposits on a backstop basin of the Hellenic Trench System (Messara Basin, Crete, Greece, was studied. The obtained pyrolysis data indicate that the containing organic matter is present in sufficient abundance and with good enough quality to be regarded as potential source rocks. The observed type III kerogen suggests gas generation potential. Although indications of higher thermal evolution occur the studied rocks suggest low maturation levels. The biogenic gas seeps in the studied research well further demonstrate the regional gas generation potential.

  2. K-Basins design guidelines

    Energy Technology Data Exchange (ETDEWEB)

    Roe, N.R.; Mills, W.C.

    1995-06-01

    The purpose of the design guidelines is to enable SNF and K Basin personnel to complete fuel and sludge removal, and basin water mitigation by providing engineering guidance for equipment design for the fuel basin, facility modifications (upgrades), remote tools, and new processes. It is not intended to be a purchase order reference for vendors. The document identifies materials, methods, and components that work at K Basins; it also Provides design input and a technical review process to facilitate project interfaces with operations in K Basins. This document is intended to compliment other engineering documentation used at K Basins and throughout the Spent Nuclear Fuel Project. Significant provisions, which are incorporated, include portions of the following: General Design Criteria (DOE 1989), Standard Engineering Practices (WHC-CM-6-1), Engineering Practices Guidelines (WHC 1994b), Hanford Plant Standards (DOE-RL 1989), Safety Analysis Manual (WHC-CM-4-46), and Radiological Design Guide (WHC 1994f). Documents (requirements) essential to the engineering design projects at K Basins are referenced in the guidelines.

  3. K-Basins design guidelines

    International Nuclear Information System (INIS)

    The purpose of the design guidelines is to enable SNF and K Basin personnel to complete fuel and sludge removal, and basin water mitigation by providing engineering guidance for equipment design for the fuel basin, facility modifications (upgrades), remote tools, and new processes. It is not intended to be a purchase order reference for vendors. The document identifies materials, methods, and components that work at K Basins; it also Provides design input and a technical review process to facilitate project interfaces with operations in K Basins. This document is intended to compliment other engineering documentation used at K Basins and throughout the Spent Nuclear Fuel Project. Significant provisions, which are incorporated, include portions of the following: General Design Criteria (DOE 1989), Standard Engineering Practices (WHC-CM-6-1), Engineering Practices Guidelines (WHC 1994b), Hanford Plant Standards (DOE-RL 1989), Safety Analysis Manual (WHC-CM-4-46), and Radiological Design Guide (WHC 1994f). Documents (requirements) essential to the engineering design projects at K Basins are referenced in the guidelines

  4. Gulf Stream Marine Hydrokinetic Energy Observations for North Carolina

    Science.gov (United States)

    Muglia, M.; Edge, B.; Lowcher, C.

    2014-12-01

    North Carolina and Florida are likely the only two states on the US east coast that have practical access to energy extraction from the Gulf Stream. After leaving the Florida Straits, the Gulf Stream in the region offshore of Cape Hatteras, NC exhibits the least variability in position of any location on the east coast, while simultaneously being closest to land. These important characteristics have made this area the focus of observations to quantify the hydrokinetic energy that may be available from the Gulf Stream for the state of North Carolina. Three types of observations to quantify the energy resource off NC began in 2013. A 150 kHz Acoustic Doppler Current Profiler (ADCP) was moored on the 225 meter isobath at the location estimated to be best for energy extraction, and recovered after a 9-month continuous deployment. Another ADCP was moored in nearly the same location to continue observations, and will be retrieved this fall. Currents from the first deployment averaged 1.15 m/s, and the average Betz Power was 0.8 kW/m2 at a depth of 30 meters over the 9-month duration. Significant variability in current speed, and thus power, occurred over the deployment period. Additionally, current measurements from a vessel mounted 300 kHz ADCP were made from water depths of 100m to 1000 m on a cross-isobath transect that included the location of the ADCP mooring. Currents from the ship transects are still under evaluation and comparison with the 150 kHz ADCP mooring, and will provide valuable information about the spatial variability of the current and its dependence on depth. A coastal ocean radar was added to an existing radar network to provide hourly surface current measurements over the larger study area. Methods to use the relative vorticity in the surface currents to identify the shoreward front of the Gulf Stream are being developed and compared with existing frontal determinations such as Navy Gulf Stream frontal charts produced bi-daily. Frontal estimates are

  5. Marketing San Juan Basin gas

    International Nuclear Information System (INIS)

    Marketing natural gas produced in the San Juan Basin of New Mexico and Colorado principally involves four gas pipeline companies with significant facilities in the basin. The system capacity, transportation rates, regulatory status, and market access of each of these companies is evaluated. Because of excess gas supplies available to these pipeline companies, producers can expect improved take levels and prices by selling gas directly to end users and utilities as opposed to selling gas to the pipelines for system supply. The complexities of transporting gas today suggest that the services of an independent gas marketing company may be beneficial to smaller producers with gas supplies in the San Juan Basin

  6. Western Canada Sedimentary Basin competitiveness

    International Nuclear Information System (INIS)

    Recent dramatic expansion of the natural gas industry in the Western Canada Sedimentary Basin provided ample proof of the potential of this area for further development of natural gas supply. However, the inherent competitive advantages provided by the Western Canada Sedimentary Basin were said to have been offset by low netback prices resulting in poor producer economics when competitiveness is measured by availability of opportunities to find and develop gas supply at costs low enough to ensure attractive returns. Technology was identified as one of the key elements in improving basin competitiveness, but the greatest potential lies in reduced transportation costs and increased access to North American market centres. 8 figs

  7. Marine archaeological exploration on the western coast, Gulf of Khambhat

    Digital Repository Service at National Institute of Oceanography (India)

    Gaur, A.S.; Bhatt, B.K.

    Cream slip Basin Black ware Jar Cream slipped Jar Grey ware Surahi Buff ware Bowl Chinese ware Basin Grey ware Dish Blue glazed Bowl Blue glazed Bowl Blue glazed Bowl Green glazed Dish Blue glazed Bowl Blue glazed Dish Brown glazed Fig. 2: Indo-Arab type...

  8. Deep Water Compositions From the Los Angeles Basin and the Origin of Formation Water Salinity

    Science.gov (United States)

    Boles, J.; Giles, G.; Lockman, D.

    2005-12-01

    Deep basin formation waters represent original depositional waters that have been modified by diagenetic processes at elevated temperatures and pressures. In addition, they may be diluted by meteoric incursion from elevated structural blocks along basin flanks. It has long been thought that deep basin formation waters have salinities greater than sea water due to various processes like clay membrane filtration or other types of water-rock interaction. However, our work and similar studies in the San Joaquin basin show that formation waters in deep basins are more likely to become diluted rather than concentrated in the absence of soluble evaporite deposits that might underlie the basin. The idea of increased salinity with depth arose from studies in which the underpinning of the basin consisted of soluble evaporate deposits such as the Texas Gulf Coast, Illinois, Michigan, and some North Sea areas. There are very few deep formation water analyses from the Los Angeles Basin. Furthermore, very few of the current produced waters from any depth can be considered pristine because of the widespread formation water injection programs and commingling of fluids from different levels. Here, we describe the first analyses from a deep, previously untouched part of the basin that is currently being developed in the Inglewood Oil Field. We have analyzed a suite of formation waters from the mid-Miocene marine Sentous sandstone from sub-sea level depths of 2250 m to 2625 m at temperatures of about 110 to 126°C and pressures of about 27 MPa. The original depositional waters in the Sentous Formation were sea water whereas the sampled waters are diluted by about 20% from sea water and some show as much as 50% dilution. Based on comparison of oxygen and deuterium isotopes between the meteoric water trend and these waters, we conclude that the smectite to illite dehydration reaction is the major cause of dilution to the original formation water. Other notable differences include

  9. First record of two hard coral species (Faviidae and Siderastreidae from Qeshm Island (Persian Gulf, Iran

    Directory of Open Access Journals (Sweden)

    MOHAMMAD SHARIF RANJBAR

    2010-01-01

    Full Text Available Moradi M, Kamrani E, Shokri MR, Ranjbar MS, Hesni MA (2009 First record of two hard coral species (Faviidae and Siderastreidae from Qeshm Island (Persian Gulf, Iran. Nusantara Bioscience 2: 34-37. Two species of hard corals including Cyphastrea chalcidicum (Forskal 1775 (Faviidae and Coscinaraea monile (Forskal 1775 (Siderastreidae were collected from the south of Qeshm Island (Persian Gulf, Iran in the late of 2008. These species were previously reported from southern Persian Gulf, Gulf of Aden, Southeast Africa and Indo-Pacific. The literature review on the distribution of these two species revealed that these species were firstly recorded from the Persian Gulf. These findings further emphasize the high diversity of coral fauna in the Iranian waters of the northern Persian Gulf.

  10. Geometry of the North Anatolian fault beneath the Gulf of Izmit and extent of the 1999 seafloor rupture

    Science.gov (United States)

    Cormier, M.-H.; Seeber, L.; Polonia, A.; Cagatay, M. N.; Emre, O.; McHugh, C. M. G.; Bortoluzzi, G.; Gorur, N.

    2003-04-01

    High-resolution multibeam bathymetry data acquired during two recent surveys clearly highlight the trace of the North Anatolian Fault beneath Izmit Gulf. The fault follows the approximate axis of the Darica (Western) Basin and the Karamürsel (Central) Basin, and has an overall orientation consistent with Present relative plate motion documented by GPS measurements. In detail, the fault displays the en echelon geometry typical of right-lateral transform faults, with right-stepping en echelon folds and left-stepping Riedel shear fractures along its strike. Seafloor relief across the fault ranges from less than 1 m to over 100 m, indicating that strike-slip motion is often associated with a component of vertical slip. Holocene submerged shorelines are visible north of the fault which do not appear affected by vertical tectonics. In contrast, the corresponding shorelines cannot be unambiguously located south of the fault,. This may partly reflect the higher sediment supply south of the fault. It also suggests most of the vertical component of slip in central and western Izmit basins is accommodated by subsidence of the southern block. The August 17, 1999 earthquake produced more than 4 m of lateral slip in Golcuk on the eastern end of Karamursel basin, but did not affect Hersek Peninsula on the western end. On the other hand, several InSAR, GPS, and seismicity analysis concur to indicate 1--2 m of slip within the subsurface west of Hersek Peninsula. Multibeam backscatter data do not reveal any disturbance in Darica and Karamursel Basins, except close to Golcuk near 29^o43'E, where sub-parallel EW lineaments and very reflective seafloor affect the entire width of the Bay. We tentatively interpret this anomalous seafloor as underwater mole tracks and dewatering features associated with the 1999 seafloor rupture. In combination with the lack of evidence for ground rupture on Hersek, acoustic backscatter data suggest that the surface rupture terminated near 29^o43'E

  11. Bio-Optical Characteristics of the Northern Gulf of California during June 2008

    OpenAIRE

    Martha Bastidas-Salamanca; Adriana Gonzalez-Silvera; Roberto Millán-Núñez; Eduardo Santamaria-del-Angel; Robert Frouin

    2014-01-01

    Bio-optical variables in the Northern Gulf of California were analyzed using in situ and satellite data obtained during a cruise in June 2008. The study area was divided into three bio-optical regions: Upper Gulf (UG), Northern Gulf (NG), and Great Isles (GI). Each region was characterized according to phytoplankton pigment concentration, phytoplankton and nonpigmented material spectral absorption coefficients, and spectral reflectance. Observed patterns were an indication of the shift in bio...

  12. Climate change and its potential impacts on the Gulf Coast region of the United States.

    Science.gov (United States)

    Tchounwou, P B

    1999-01-01

    The Gulf Coast region of the United States abuts five states, including Alabama, Florida, Louisiana, Mississippi, and Texas. In general, the Gulf of Mexico has a surface area of 1.63 million square kilometers (630,000 square miles) and a watershed area of 4.69 million square kilometers (1.81 million square miles) in the United States. This region is one of the nation's largest ecological systems and is closely linked to a significant portion of the nation's economy. In the Gulf Coast region, energy, fisheries, agriculture, and tourism rank among the most significant sectors of the economy. The Gulf has five of the top ten fishing ports in the United States, and commercial fisheries in the Gulf annually produce nearly 2 billion tons of fish, oysters, shrimps, and crabs. Gulf ports handle one-half of the nation's import-export tonnage. Petroleum produced in the Gulf represents about 80% of the nation's offshore production. The Gulf Coast region largely relies on many natural resources to fuel many important sectors of its economy. But nevertheless, the health and vitality of the Gulf have declined in recent years, caused in part by increasing populations along its coast and the growing demand upon its resources and in part by the accumulation of years of careless depletion, abuse, and neglect of the environment. Equally important are the impacts of natural and human-induced climate change on the economy and on the quality of life for millions of people living in the Gulf Coast region. The results have generated alarming increases in damage to and destruction of the ecosystems and habitats of the Gulf. This paper reviews the nature of global environmental change and addresses the potential health and environmental impacts that may occur in the Gulf Coast region of the United States as a consequence of various environmental alterations resulting from global change. PMID:10485132

  13. A reappraisal of postglacial decay times from Richmond Gulf and James Bay, Canada

    OpenAIRE

    J.X. Mitrovica; Forte, A. M.; M. Simons

    2000-01-01

    Decay times inferred from relative sea-level (RSL) histories of previously glaciated regions provide a potentially important constraint on mantle rheology. We present a new compilation of RSL data from Richmond Gulf and James Bay, Canada. This recompilation reveals errors in previous compilations that led to inaccurate estimates for the Richmond Gulf decay time in a series of recently published articles. We derive updated estimates for the decay time at Richmond Gulf and James Bay using a met...

  14. Intravenous drug abuse and tricuspid valve endocarditis: Growing trends in the Middle East Gulf region

    OpenAIRE

    Panduranga, Prashanth; Al-Abri, Seif; Al-Lawati, Jawad

    2013-01-01

    Traditionally, tricuspid valve endocarditis is uncommon in the Middle East region. However, recent global data indicate growing trends in the use of illicit drug abuse, specifically injectable heroin, in the Middle East Gulf region. The presence of many transit port services in the Middle East Gulf States has led to smuggling of substance abuse drugs in the region. The Middle East Gulf States, currently a transit market, are also becoming a growing consumer market in view of the increased sub...

  15. Trip report Rainwater Basin Nebraska

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — This report is a summary a trip to Rainwater Basin Wetland Management District in 1991, and focuses on the hydrology and soil habitat types. It is part of the...

  16. Allegheny County Basin Outlines Map

    Data.gov (United States)

    Allegheny County / City of Pittsburgh / Western PA Regional Data Center — This basins dataset was created to initiate regional watershed approaches with respect to sewer rehabilitation. If viewing this description on the Western...

  17. Geological and hydrological exploration of Gulf Coast Salt Domes

    International Nuclear Information System (INIS)

    The geologic exploration program in the Gulf Coast Salt Dome Region is based on a screening process that includes a series of increasingly detailed studies. The screening procedure takes the following steps: (1) determination of regions for further study (in this case, the salt domes of the interior Gulf Coast); (2) regional surveys and the determination of areas within those regions which are thought to be most suitable and which are recommended for further evaluation (in this case, eight specific salt domes); (3) area characterizations and the determination of locations within the areas which are thought to have a high probability of suitability (in this case, two or three of the eight salt domes); (4) location studies and the determination of a potential repository site, which is thought to be suitable and licensable and which is recommended for completion of site characterization studies

  18. Macro-Ecology of Gulf of Mexico Cold Seeps

    Science.gov (United States)

    Cordes, Erik E.; Bergquist, Derk C.; Fisher, Charles R.

    2009-01-01

    Shortly after the discovery of chemosynthetic ecosystems at deep-sea hydrothermal vents, similar ecosystems were found at cold seeps in the Gulf of Mexico. Over the past two decades, these sites have become model systems for understanding the physiology of the symbiont-containing megafauna and the ecology of seep communities worldwide. Symbiont-containing bivalves and siboglinid polychaetes dominate the communities, including five bathymodiolin mussel species and six vestimentiferan (siboglinid polychaete) species in the Gulf of Mexico. The mussels include the first described examples of methanotrophic symbiosis and dual methanotrophic/thiotrophic symbiosis. Studies with the vestimentiferans have demonstrated their potential for extreme longevity and their ability to use posterior structures for subsurface exchange of dissolved metabolites. Ecological investigations have demonstrated that the vestimentiferans function as ecosystem engineers and identified a community succession sequence from a specialized high-biomass endemic community to a low-biomass community of background fauna over the life of a hydrocarbon seep site.

  19. Research on the Seismotectonic Setting in Beibu Gulf Waters

    Institute of Scientific and Technical Information of China (English)

    Li Jinchen; Pan Hua; Chen Wenbin

    2010-01-01

    In this paper we discuss the seismogenic structures of the two earthquakes occurring in the Beibu Gulf waters,based on the investigation of geological structure,faults,geophysical fields,seismicity and earthquake focal mechanism.The results show that the NEE trending faults along the boundary of the Wushi depression are the dominating seismogenic structures,and the NW trending faults are the key factors of stress concentration.The results also show that high seismicity has a significant relationship with the late Cenozoic deposition center in the Beibu Gulf,and their NE-NEE trending boundary faults are important to the identification of seismogenic structures.The special arcuate fault segment or the intersection point of the NW trending faults and NE-NEE trending boundary faults is a possible location of future earthquakes.

  20. Gulf of Mexico Helicopter Offshore System Technologies Recommended Development Path

    Science.gov (United States)

    Koenke, Edmund J.; Williams, Larry; Calafa, Caesar

    1999-01-01

    The National Aeronautics and Space Administration (NASA) Advanced Air Transportation Technologies (AATT) project in cooperation with the Department of Transportation (DOT) Volpe National Transportation Systems Center (VNTSC) contracted with the System Resources Corporation (SRC) for the evaluation of the existing environment and the identification of user and service provider needs in the Gulf of Mexico low-altitude Offshore Sector. The results of this contractor activity are reported in the Gulf of Mexico Helicopter Offshore System Technologies Engineering Needs Assessment. A recommended system design and transition strategy was then developed to satisfy the identified needs within the constraints of the environment. This work, also performed under contract to NASA, is the subject of this report.