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Abstract

The Rhodanian-Provencal Basin is the southernmost part of the Peri-Alpine Seaway developed during the Miocene from Austria to the Mediterranean Sea (Fig. 1). This basin is located in a peripheral or external domain of the Western Alps foreland basin. Flexural subsidence related to alpine thrust loading provides accomodation space.

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/content/papers/10.3997/2214-4609.201405981
2000-10-01
2021-07-30
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201405981
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