On the trail of a major trans-Tethyan discontinuity

At the base of the Valanginian a major discontinuity associated with one of the major transgressions of the Cretaceous is nominated as a candidate for the boundary between the Cretaceous and Jurassic systems. This surface has been identified in both platform and basinal domains, at the eastern edge...

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Bibliographic Details
Main Author: Granier Bruno
Format: Article
Language:English
Published: Association Carnets de Geologie 2007-05-01
Series:Carnets de Géologie
Subjects:
Online Access:http://paleopolis.rediris.es/cg/CG2007_M02/CG2007_M02_Abstract07.html