Sedimentation and palaeogeography of the eastern part of the Paris Basin France at the Middle-Upper Jurassic boundary

Titre Sedimentation and palaeogeography of the eastern part of the Paris Basin France at the Middle-Upper Jurassic boundary
Titre court Sedimentation and palaeogeography of the eastern part of the Paris Basin France at the Middle-Upper Jurassic boundary
Type de document article
Auteur(s) Collin, P.-Y.
Courville, P.
Date 2006
Titre de la publication Comptes Rendus Geoscience
Volume 338
12-13
N° de page(s) 824-833
Résumé The Middle–Upper Jurassic boundary corresponds to a period of far-reaching changes in sedimentation patterns related to alterations in the palaeoclimate and in the global carbon cycle. Marl deposits were laid down in the east of the Paris Basin at this time and ANDRA has selected these lithological units as the site for an underground study laboratory. The build-up of these marls is the result, among other things, of the area long having been a shelf and of more rapid subsidence from the Early Callovian to the Early Oxfordian. Changes are detected between areas on either side of the Vittel Fault from the onset of the mid-Oxfordian onwards.
Planches et figures 4 figs
Site http://www.sciencedirect.com/science/article/pii/S163107130600229X
DOI 10.1016/j.crte.2006.07.011
Langue Français
Collection Notre bibliothèque
Collin, P.-Y. and Courville, P., 2006. Sedimentation and palaeogeography of the eastern part of the Paris Basin France at the Middle-Upper Jurassic boundary. Comptes Rendus Geoscience. 338 n° 12-13. p. 824-833. 4 figs. Site : .

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