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pro vyhledávání: '"Antoine Crémades"'
Tectono-stratigraphic evidence of salt tectonics during Jurassic extension in the Corbières nappe, Eastern Pyrenees, France Antoine Crémades1, Mary Ford1 et Julien Charreau11 CRPG, UMR 7358 CNRS, Université de Lorraine, Vandoeuvre‐lès‐Nancy,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7fc4e0c621997392b7df0b306bdcf6df
https://doi.org/10.5194/egusphere-egu2020-6716
https://doi.org/10.5194/egusphere-egu2020-6716
Autor:
Mary Ford, Emmanuel Masini, Jaume Vergés, Raphael Pik, Sébastien Ternois, Julien Léger, Armin Dielforder, Gianluca Frasca, Arjan Grool, Constance Vinciguerra, Thomas Bernard, Paul Angrand, Antoine Crémades, Gianreto Manatschal, Sébastien Chevrot, Laurent Jolivet, Frédéric Mouthereau, Isabelle Thinon, Sylvain Calassou
Publikováno v:
Bulletin de la Société Géologique de France
Bulletin de la Société Géologique de France, 2022, 193, pp.19. ⟨10.1051/bsgf/2022018⟩
Bulletin de la Société Géologique de France, 2022, 193, pp.19. ⟨10.1051/bsgf/2022018⟩
[EN]: The Pyrenees is a collisional orogen built by inversion of an immature rift system during convergence of the Iberian and European plates from Late Cretaceous to late Cenozoic. The full mountain belt consists of the pro-foreland southern Pyrenee