1887

Abstract

The cast-west trending Pyrenees-Provence thrust belt developed from late Cretaceous to early Tertiary times in response to the north-south convergence of the Iberian and European plates. Post-tectonic sedimentary basins started developing in late Eocene times over the eastern half of the belt in response to the rifting and opening of the Western Mediterranean oceanic basin.

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/content/papers/10.3997/2214-4609.201410271
1994-06-10
2020-04-02
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201410271
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