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161.
162.
Maurice Recq Jean-Pierre Rehault Gilbert Bellaiche Maurice Gennesseaux Jean-Pierre Esteve 《Earth and Planetary Science Letters》1976,28(3):323-330
Offshore seismic refraction profiles permitted us to characterize the extent of the geological formations which prolong the principal units of the Provence and Alpes Maritimes southwards and to establish their respective relationships. The concept of a “Var graben” is confirmed and defined. A magma chamber, probably in relation with the volcanic deposits of the Cap d'Ail, has been disclosed and coincides with the positive magnetic anomaly observed in this area. 相似文献
163.
164.
165.
166.
Sediment community metabolism associated with continental shelf hypoxia, Northern Gulf of Mexico 总被引:1,自引:0,他引:1
Gilbert T. Rowe Marta Elizabeth Cruz Kaegi John W. Morse Gregory S. Boland Elva G. Escobar Briones 《Estuaries and Coasts》2002,25(6):1097-1106
Net fluxes of respiratory metabolites (O2, dissolved inorganic carbon (DIC), NH4 +, NO3 ?, and NO2 ?) across the sediment-water interface were measured using in-situ benthic incubation chambers in the area of intermittent seasonal hypoxia associated with the Mississippi River plume. Sulfate reduction was measured in sediments incubated with trace levels of35S-labeled sulfate. Heterotrophic remineralization, measured as nutrient regeneration, sediment community oxygen consumption (SOC), sulfate reduction, or DIC production, varied positively as a function of temperature. SOC was inversely related to oxygen concentration of the bottom water. The DIC fluxes were more than 2 times higher than SOC alone, under hypoxic conditions, suggesting that oxygen uptake alone cannot be used to estimate total community remineralization under conditions of low oxygen concentration in the water column. A carbon budget is constructed that compares sources, stocks, transformations, and sinks of carbon in the top meter of sediment. A comparison of remineralization processes within the sediments implicates sulfate reduction as most important, followed by aerobic respiration and denitrification. Bacteria accounted for more than 90% of the total community biomass, compared to the metazoan invertebrates, due presumably to hypoxic stress. 相似文献
167.
Jennifer M. Cole E. Troy Rasbury† Isabel P. Montañez‡ Vicki A. Pedone§ Antonio Lanzirotti¶ Gilbert N. Hanson† 《Sedimentology》2004,51(3):433-453
An integrated petrographic and spectroscopic (X‐ray diffraction, phosphor imaging and synchrotron X‐ray absorption spectroscopy) study of tufas from the Miocene Barstow Formation, California, relates sample morphology, mineralogy and geochemical composition. The tufas, composed mainly of calcite that formed at the interface between an ancient alkaline lake and ground or spring waters, have textures similar to those of microbially mediated terrestrial stromatolites and travertines. The tufas have elevated concentrations of a number of trace elements including Mn, Fe, Sr and U. Synchrotron X‐ray fluorescence analyses show that U concentrations can exceed 500 p.p.m. X‐ray absorption spectroscopy indicates that the U in these samples is incorporated as U(IV). It is suggested here that alkaline lake waters had a high U/Ca ratio and tufa calcite formed where groundwater or (possibly epithermal) springs brought in Ca and trace elements such as Sr. The rapid, and possibly microbially mediated, precipitation of calcite allowed for incorporation of high concentrations of trace metals as either structural substitutes or extremely fine‐scale inclusions. 相似文献
168.
Katja Deckart Gilbert F raud Herv Bertrand 《Earth and Planetary Science Letters》1997,150(3-4):205-220
A detailed 40Ar/39Ar study, of mineral separates from the Jurassic Atlantic Continental Tholeiites (JACT) of Guyana (French Guyana and Surinam, South America), and Guinea (West Africa) related to the initial opening of the Central Atlantic, has been carried out. In French Guyana, plateau ages of 196.0 ± 5.7 Ma and 196.1 ± 7.5 Ma were obtained on single, small amphibole grains from NNW—SSE trending dykes. In Guinea, single biotite grains from intrusive formations from the Kakoulima and Fouta Djalon areas yielded plateau ages of 200.4 ± 0.2 Ma and 194.8 ± 0.5 Ma, concordant with high temperature apparent ages on other biotites. The bulk plagioclase samples display disturbed age spectra due to alteration and excess argon. However, intermediate temperature, weighted mean plagioclase ages are similar in both regions of Guyana and Guinea, ranging from 200.2 ± 2.4 Ma to 188.7 ± 1.9 Ma, partly in agreement with the amphibole and biotite data.
These data, combined with previous 40Ar/39Ar and U/Pb results from the northern part of the Central Atlantic margins, indicate intense magmatic activity distributed over a large area from Iberia to Liberia (ca. 4500 km long) for a short period of time (204-195 Ma, perhaps less for the bulk of the magmatism) during the initial break-up of Pangea continent. These data do not support an initiation of the magmatism from a radial volcano-tectonic system centred in the south of the region, as suggested by May [1], and the initial break-up seems to affect the whole Central Atlantic during a period of 9 Ma. 相似文献
169.
John K. Zachariah V. Rajamani Gilbert N. Hanson 《Contributions to Mineralogy and Petrology》1997,129(1):87-104
The N–S trending, 2–4 km wide Ramagiri schist belt is made up of three blocks dominated by metavolcanic rocks, separated
and surrounded by granitic rocks of distinct characteristics. The metavolcanic rocks are tholeiitic in composition and are
very similar in their major element composition as well as in their abundances of some trace elements. However, the rare earth
elements (REE) require distinct sources. The rocks of the amphibolite facies eastern block have LREE depleted REE patterns
([Ce/Yb] = 0.7–0.9), requiring derivation from depleted mantle-like sources. The greenschist facies metatholeiitic rocks of
the central block have LREE enriched REE patterns ([Ce/Yb] = 3–6), reflecting the nature of their source(s). The Nd isotopic
data require that the LREE enriched nature could not have been attained significantly prior to its melting. The fine-grained,
upper greenschist facies metatholeiites of the western block have flat to slightly LREE depleted patterns ([Ce/Yb] = 0.8–0.95).
Minor fractional crystallization of rock forming minerals may relate a few samples to each other among samples from each of
the three blocks. Different extents of partial melting of distinct mantle sources have played a dominant role in the generation
of the parent magmas to the central versus eastern and western block metatholeiites.
The geochemical data suggest that the mantle sources were non-lherzolitic, and that these sources may have seen previous episodes
of melt addition and extraction prior to melting that gave rise to the parent melts to the rocks ∼2750 Ma ago. The REE data
indicate that while the sources of the eastern and western block rocks were similar to depleted mantle (ɛNd(
i
) about +2), the source of the central block rocks (ɛNd(
i
) about +3.5) were enriched in large ion lithophile element (LILE)-rich fluids/melts probably derived from subducting oceanic
crust. This and other trace element signatures point to magma extraction in tectonic settings similar to modern island arcs.
Subsequent to magma emplacement and crystallization, all the three suites of rocks were affected by interaction with low-temperature,
crustal derived fluids (ɛNd 2750Ma of about −8 to −12), probably during the accretion of the three blocks of the belt in the present form. The inferred source
characteristics, tectonic setting of magma generation and the crustal fluid processes seem to suggest that Phanerozoic-style
tectonic processes may have been important in the generation of Archean crust in the Dharwar craton.
Received: 31 July 1995 / Accepted: 12 May 1997 相似文献
170.
Urs Schrer Jacques Kornprobst Marie-Odile Beslier Gilbert Boillot Jacques Girardeau 《Earth and Planetary Science Letters》1995,130(1-4)
The thinned continental crust of the west Galicia margin is bound by a belt of serpentinized peridotites (‘peridotite ridge’) lying about 300 km off the coast in the North Atlantic ocean. From this ridge, a gabbro and a chlorite rock were studied in an attempt to substantiate rift-related subcontinental magmatism, occurring prior to sea-floor spreading. U-Pb dating of 13 different zircon fractions yields a precise age of 122.1 ± 0.3 Ma (2σ) for the emplacement of the chlorite rock protolith, from which more than 50% of Si and alkali-calc-alkali elements were lost during greenschist facies tectonometamorphism. Sr and Nd isotope signatures suggest that the gabbro and chlorite rock protoliths were derived from mantle sources that were moderately depleted in LILE, relative to a chondritic reservoir. No evidence for the presence of continental material in the magma source regions can be observed. From the new zircon age of 122.1 ± 0.3 Ma, and earlier determined39Ar40Ar age of 122.0 ± 0.6 Ma for amphibole from the same locality, it can be documented that magma formation, solidification and unroofing of the mantle rocks occurred during a short period of time of about 3.4 Ma, which means that the peridotite ridge detached from the continent and rose to the surface immediately after, or even coevally with mantle melting. 相似文献