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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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Springer
2016-04-01
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| Col·lecció: | Terrestrial, Atmospheric and Oceanic Sciences |
| Matèries: | |
| Accés en línia: |
http://tao.cgu.org.tw/pdf/v272p203.pdf
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