Search results for "Variscan orogeny"

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U-Pb age constraints on Carboniferous-Permian French continental basins - implications for their depositional history and correlations with European …

2022

International audience; Late Carboniferous to Permian basins of western Europe (~Gzhelian to Artinskian), developed during thelate stages of the Variscan orogeny in equatorial paleolatitudes. The stratigraphic context of most of thesebasins remains poorly constrained, because mainly based on “continental stages” (e.g., Stephanian, Autunian,Saxonian and Thuringian) that are diachronous. Therefore, correlating these basins together and withinternationally recognized stratigraphic marine stages requires precise radiochronologic ages.To the south of the Paris Basin (France), volcanic ash-fall layers (i.e., tonsteins) are interbedded in theCarboniferous-Permian sedimentary successions of the Aum…

[SDU.STU.GC]Sciences of the Universe [physics]/Earth Sciences/Geochemistrycontinental Pangea basins[SDU.STU.ST]Sciences of the Universe [physics]/Earth Sciences/Stratigraphy[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry[SDU.STU.ST] Sciences of the Universe [physics]/Earth Sciences/Stratigraphylate PaleozoicVariscan orogeny
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Fusulines of the Hoyo Oscuro section, Ándara massif of Picos de Europa (Cantabrian Zone, N Spain). New constraints about the onset of the Variscan de…

2020

The Hoyo Oscuro section (Andara Massif, southeastern part of Picos de Europa) is a comparatively small exposure of Pennsylvanian syntectonic deposits that shown angular unconformity on the fairly extensive pre-tectonic carbonate platform strata of Pennsylvanian age accumulated in the distalmost realms of the Variscan foreland basin of the Cantabrian Zone. Fusuline-bearing strata from this section yielded species belonging to the genera P seudostaffella, Ozawainella, Fusulinella, Protriticites, Pseudotriticites, Fusulina and Quasifusulinoides ; one of these forms, Protriticites schulzei Villa, is described as a new species from the Cantabrian Mountains. Fusuline assemblages allow us to corre…

geographygeography.geographical_feature_categoryAnchor pointCarbonate platformPaleontologyOrogenyMassifQE701-760UnconformityPaleontologySection (archaeology)PennsylvanianForeland basinGeologyfusulines carboniferous (pennsylvanian) cantabrian zone variscan orogeny picos de europa
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