Search results for "palaeovolcanism"

showing 2 items of 2 documents

The first 40Ar-39Ar date from Oxfordian ammonite-calibrated volcanic layers (bentonites) as a tie-point for the Late Jurassic.

2013

AbstractEight volcanic ash layers, linked to large explosive events caused by subduction-related volcanism from the Vardar Ocean back-arc, interbedded with marine limestones and cherts, have been identified in the Rosso Ammonitico Veronese Formation (northeastern Italy). The thickest ash layer, attributed to the Gregoryceras transversarium ammonite Biozone (Oxfordian Stage), yields a precise and reliable 40Ar–39Ar date of 156.1 ± 0.89 Ma, which is in better agreement with GTS2004 boundaries than with the current GTS2012. This first biostratigraphically well-constrained Oxfordian date is proposed as a new radiometric tie-point to improve the Geologic Time Scale for the Late Jurassic, where a…

010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesgeochronologyBiozone010502 geochemistry & geophysics[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy01 natural sciencesOxfordianPaleontologyGeologic time scale[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/GeochemistryStage (stratigraphy)0105 earth and related environmental sciencesAmmonitegeographygeography.geographical_feature_categorypalaeovolcanismbentoniteGeology[ SDU.STU.GC ] Sciences of the Universe [physics]/Earth Sciences/Geochemistrylanguage.human_languageJurassic Time Scale[ SDE.MCG ] Environmental Sciences/Global ChangesVolcano[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeochronologylanguageRadiometric datingGeologyVolcanic ash
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Mineralogical variability of Callovo-Oxfordian clays from the Paris Basin and the Subalpine Basin.

2006

High-resolution clay mineralogical data at the Middle/Upper Jurassic boundary from the French Subalpine Basin, the Jura Mountains and the Paris Basin (ANDRA boreholes) from Callovo-Oxfordian clayey deposits allow spatial and temporal terrigenous flux evolution to be considered over a period of 6 to 7 Myr. Recorded diachronisms of major mineralogical changes and complex clays distribution at the Paris Basin scale result to combined palaeogeographic/eustatic variations and climate input. In the French Subalpine Basin, mineralogical homogeneity confirms the burial diagenesis influence, but other terrigenous supplies must be involved in contrast to the Paris Basin domains. Volcanogenic clays (b…

Bentonites010504 meteorology & atmospheric sciences[SDE.MCG]Environmental Sciences/Global ChangesCallovian[ SDU.STU.VO ] Sciences of the Universe [physics]/Earth Sciences/VolcanologyBiostratigraphyStructural basin[ SDU.STU.ST ] Sciences of the Universe [physics]/Earth Sciences/Stratigraphy010502 geochemistry & geophysics01 natural sciencesOxfordianPaleontologyPalaeovolcanismParis Basin[SDE.MCG.CG]Environmental Sciences/Global Changes/domain_sde.mcg.cgPhanerozoic[SDU.STU.VO]Sciences of the Universe [physics]/Earth Sciences/Volcanology[ SDE.MCG.CG ] Environmental Sciences/Global Changes/domain_sde.mcg.cg[ SDU.STU.MI ] Sciences of the Universe [physics]/Earth Sciences/Mineralogy0105 earth and related environmental sciencesGlobal and Planetary ChangeTerrigenous sedimentDiagenesisClay minerals[ SDE.MCG ] Environmental Sciences/Global Changes13. Climate actionClastic rock[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/StratigraphyGeneral Earth and Planetary SciencesSedimentary rockFrancePalaeogeographyGeologyVolcanic ash[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
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