Poly-phased fluid flow in the giant fossil pockmark of Beauvoisin, SE basin of France

Poly-phased fluid flow in the giant fossil pockmark of Beauvoisin, SE basin of France

The giant Jurassic-aged pockmark field of Beauvoisin developed in a 800 m wide depression for over 3.4 Ma during the Oxfordian; it formed below about 600 m water depth. It is composed of sub-sites organized in clusters and forming vertically stacked carbonate lenses encased in marls . This fine-scal...

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Bibliographic Details
Main Authors: Gay Aurélien, Favier Alexiane, Potdevin Jean-Luc, Lopez Michel, Bosch Delphine, Tribovillard Nicolas, Ventalon Sandra, Cavailhes Thibault, Neumaier Martin, Revillon Sidonie, Travé Anna, Bruguier Olivier, Delmas Doriane, Nevado Christophe
Format: Article
Language:English
Published: EDP Sciences 2020-01-01
Series:BSGF - Earth Sciences Bulletin
Subjects:
focused fluid flow
basin geology
pockmark
beauvoisin
tethyan margin
oxfordian
Online Access:https://www.bsgf.fr/articles/bsgf/full_html/2020/01/bsgf200003/bsgf200003.html

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