Les formations burdigaliennes de Corse orientale dans leur cadre géodynamique |
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Authors: | Marie-Dominique Loÿe-Pilot Michel Durand-Delga Hugues Feinberg Yves Gourinard Jean Magné |
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Affiliation: | 1. Département « Terre, Océan, Atmosphère », École normale supérieure, 24, rue Lhomond, 75230 Paris cedex 05, France;2. La Pélisserie, 81150 Florentin, France;3. Laboratoire de géologie, École normale supérieure, 24, rue Lhomond, 75230 Paris cedex 05, France;4. Laboratoire de dynamique des bassins sédimentaires, université Paul-Sabatier, 39, allées Jules Guesde, 31062 Toulouse cedex 4, France |
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Abstract: | The earliest marine sediments of eastern Corsica, linked to the birth of the Corsica Basin, are represented by granitic breccia of the Saint-Antoine Formation and pelagic marls of the Alzelle Formation. They are dated as Mid-Burdigalian by nannoplankton and planktonic foraminifera (relative age and grade datings between 18.7 and 18.3 Ma). The Aghione Formation (Latest Burdigalian–Langhian) lies upon the Alzelle Formation. A component of the major East-Corsican faults, the Saint-Antoine Fault, underwent extensional activity during the Burdigalian and until the Late Miocene, when occurred the uplift of the Castagniccia antiform. To cite this article: M.-D. Loÿe-Pilot et al., C. R. Geoscience 336 (2004). |
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Keywords: | Corse orientale Burdigalien Langhien Foraminifères nannoplancton faille listrique granite de Linguizzetta eastern Corsica Burdigalian Langhian Foraminifera nannoplankton grade-dating listric fault Linguizzetta granite |
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