Structuration cassante de la marge vendéenne au Lias inférieur : exemple de l'estuaire du Payré au sud de Talmont-Saint-Hilaire

  • In the Talmondais (Vendée) the Hettangian sedimentation locally begins with fluviatil clastic deposits prior to the deposition of shallow marine carbonates. These clastics, including the footprint-bearing beds of Le Veillon (south of Talmont- Saint-Hilaire) are subject to important and frequent variations in thickness. Drilling and geophysic data indicate a tectonic control of these variations. A fault-block pattern is proposed. At a small scale, it gives an illustration of the extensional tectonic processes related to the evolution of the Biscay rift during the early Liassic.

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Metadaten
Author:Christian Montenat, Gilbert Bessonnat, Claude Roy
URN:urn:nbn:de:hebis:30:3-306167
Parent Title (French):Le Naturaliste Vendéen
Document Type:Article
Language:French
Date of Publication (online):2013/07/02
Year of first Publication:2003
Publishing Institution:Universitätsbibliothek Johann Christian Senckenberg
Release Date:2013/07/02
Volume:3
Page Number:9
First Page:29
Last Page:37
HeBIS-PPN:347497411
Dewey Decimal Classification:5 Naturwissenschaften und Mathematik / 55 Geowissenschaften, Geologie / 550 Geowissenschaften
Sammlungen:Sonstige
Zeitschriften / Jahresberichte:Naturaliste Vendéen / Le Naturaliste Vendéen, Numéro 3 (2003)
:urn:nbn:de:hebis:30:3-306130
Licence (German):License LogoDeutsches Urheberrecht