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Abstract

In the external Alps of SE France, Eocene-Miocene foreland basins are preserved in a series of well exposed isolated fragments (often thrust sheet top basins) which contain progressively younger sediments towards the foreland.

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/content/papers/10.3997/2214-4609.201409728
1995-05-29
2024-03-19
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201409728
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