On Land Evidence of Ligurian Margin Normal Faults at St-Jean Cap-Ferrat (France)

The French Riviera has witnessed a succession of E-W trending compressions during the Oligocene period and a N-S trending compression during the Mio-Pliocene. The presence of the Ligurian Sea and drifting of the Corsica block are due to a NW-SE trending Oligo-Miocene extension. The markers of each c...

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Bibliographic Details
Published in:	Terrestrial, Atmospheric and Oceanic Sciences
Main Author:	Lionel Sonnette
Format:	Article
Language:	English
Published:	Springer 2016-04-01
Subjects:	Brittle tectonic Fault Stress tensor French Riviera Ligurian Basin
Online Access:	http://tao.cgu.org.tw/pdf/v272p203.pdf

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