From late Visean to Stephanian: pinpointing a two-stage basinal evolution in the Variscan belt. A case study from the Bosmoreau basin (French Massif Central) and its geodynamic implications |
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| Authors: | Email author" target="_blank">O?BruguierEmail author J?F?Becq-Giraudon N?Clauer H?Maluski |
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| Institution: | (1) Service ICP-MS, cc 056, ISTEEM, Université de Montpellier II, Place E. Bataillon, 34095 Montpellier, France;(2) BRGM, 3 Avenue C. Guillemin, BP 6009, 45060 Orléans, France;(3) CGS-EOST, Université Louis Pasteur-CNRS, 1 rue Blessig, 67084 Strasbourg, France;(4) Laboratoire de Géophysique, Tectonique et Sédimentologie, CNRS-UMR 5573, ISTEEM, Université de Montpellier II, Place E. Bataillon, 34095 Montpellier, France |
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| Abstract: | Post-convergence evolution of the Variscan belt is characterized by the development of intramontane coal-bearing basins containing volcano-sedimentary successions. In the French Massif Central, K––Ar ages on clay particles from fine-grained sediments of the Bosmoreau basin (Limousin area), help pinpoint the evolution of the basin. In the lower part of the sedimentary pile, illite in a siltstone underlying a volcanic layer previously dated at 332±4 Ma by the U––Pb method on zircon, yields a consistent K––Ar age of ca. 340 Ma. Upward in the sedimentary succession, illite yields Stephanian K––Ar ages, which can be combined to provide a mean deposition age of 296.5±3.5 Ma. The Bosmoreau basin, albeit mainly filled with Stephanian deposits, was initiated during the late Visean, i.e. ca. 30 Ma earlier than inferred from biostratigraphical constraints. During the Stephanian, the same structure was reactivated and late Visean deposits were eroded and subsequently blanketed by thick clastic sediments. These results emphasise a two-stage evolution for the Bosmoreau basin, which is closely related to extensional tectonics identified on basement country rocks, and they are used to propose a geodynamic evolution of the studied area. |
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