Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
The West European collisional Alpine belts are the result of the inversion, initiated in the middle Cretaceous, of the complex western Neotethys and the Atlantic continental rift domains and closure of remnants of Tethys between the North Africa and European cratons. While the kinematics of Africa r...
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| Formato: | article |
| Lenguaje: | EN FR |
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EDP Sciences
2021
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| Acceso en línea: | https://doaj.org/article/5da653464e024ae78fc88fd01d04e3e0 |
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