6533b836fe1ef96bd12a08d5

RESEARCH PRODUCT

Tectono-biosedimentary recordings at the Lias-Dogger transition: example of the Quercy carbonate platform (Aquitaine Basin, France).

Christophe DurletPhilippe FauréJean-françois DeconinckThierry PelissieCarine LézinJacques ReyRené Cubaynes

subject

QuercyAalenian010504 meteorology & atmospheric sciencesCarbonate platform[SDE.MCG]Environmental Sciences/Global Changes[SDU.STU.TE] Sciences of the Universe [physics]/Earth Sciences/TectonicsToarcianStructural basin010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesPaleontologyStatistical processing0105 earth and related environmental sciences[SDU.STU.TE]Sciences of the Universe [physics]/Earth Sciences/Tectonicsgeographygeography.geographical_feature_categoryTectonicsGeology[ SDU.STU.TE ] Sciences of the Universe [physics]/Earth Sciences/TectonicsSedimentary basinTectonics[ SDE.MCG ] Environmental Sciences/Global ChangesCarbonate platform[SDE.MCG] Environmental Sciences/Global Changes[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyFacies[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/StratigraphyFranceSedimentationGeology

description

AbstractOn the eastern edge of the Aquitaine Basin, the Lias-Dogger transition and the events, which occurred during this time interval are studied in the Quercy sedimentary basin. Stratigraphic correlations are proposed using a biochronological calibration based on the determination of numerous ammonites and brachiopods. Facies analyses using statistical processing integrate the presence of faults and tectonic compartments and lead to reconstruction of palaeoenvironments in space and time. The paper includes the description of system tracts following Haq et al. [1987] and Vail et al. [1991], and twelve palaeogeographic maps of the area studied. The objectives are to distinguish the various allocyclic and autocyclic factors controlling sedimentation and to show the impact of the Mid-Cimmerian tectonic event on the evolution of the basin.

https://hal.science/hal-00199948