Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinema...
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
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Paris: EDP Sciences
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Language
English
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Paris: EDP Sciences
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Contents
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 relative to Europe is well understood, the kinemati...
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Full title
Evolution of the Alpine orogenic belts in the Western Mediterranean region as resolved by the kinematics of the Europe-Africa diffuse plate boundary
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TN_cdi_doaj_primary_oai_doaj_org_article_5da653464e024ae78fc88fd01d04e3e0
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_5da653464e024ae78fc88fd01d04e3e0
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ISSN
1777-5817,0037-9409
E-ISSN
1777-5817
DOI
10.1051/bsgf/2021031
