Search results for "Propriétés réservoirs"

showing 2 items of 2 documents

Structures de déformation induites par surpressions de fluide dans les environnements sous-glaciaires et marin profonds : implications paléoenvironne…

2014

Soft-sediment deformation structures (SSDs) occur in unconsolidated sediments, during or shortly after deposition. SSDs are abundant in subglacial and deep-marine environments because of the development of fluid overpressure. Case studies of these two sedimentary environments were used (1) to reconstruct palaeoenvironments from SSDS, and (2) to define the impacts of SSDS on glacial morphologies and (3) petrophysical properties.(1) Analyses of strain regimes, deformation mechanisms, and chronologies in SSDs served to improve palaeoenvironmental reconstructions. These structures were used as proxys to estimate variations of ice flow velocities, ice thickness, meltwater production, and positio…

Reconstructions paléoenvironnementalesEnvironnement marin profondFluid pressureDeep-water environment[SDU.STU]Sciences of the Universe [physics]/Earth SciencesEnvironnement sous-glaciaireVallées tunnels[ SDU.STU ] Sciences of the Universe [physics]/Earth SciencesPalaeoenvironmental reconstructionsPropriétés réservoirsPression de fluide[SDU.STU] Sciences of the Universe [physics]/Earth SciencesSubglacial environmentTunnel valleysReservoir propertiesStructures de déformation pré-lithificationSoft-sediment deformation structures
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Sedimentological and diagenetic influences on low permeability properties of the Middle Jurassic limestones (Paris Basin, France)

2009

A detailed sedimentological, geochemical and mineralogical study is carried out on the Early Bajocian to Early Callovian (Middle Jurassic) limestones of the Paris Basin. Deposits include 18 lithofacies which are stacked into 10 third-order depositional sequences. Our geochemical study including a compilation of bibliographic data allows us to refine the existing sea surface palaeotemperature pattern. A cooling from the latest Early Bajocian to the Late Bajocian and a subsequent warming from the earliest Callovian to the Early/Middle Callovian transition are described using a proxy of sea surface temperatures. Together with δ13C and mineralogical data, our new δ18O values suggest a palaeo-cl…

carbonatereservoirPétrophysiqueSédimentologieGéochimie minérale[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/GeochemistrypretrophysicSedimentologydiagenesisDiagenèsePropriétés réservoirsgeochemistry[SDU.STU.MI] Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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