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Structure of an intraplate fold-and-thrust belt: The Iberian Chain. A synthesis

The Iberian Chain is a complex intraplate fold-and-thrust belt resulting from the convergence between the Eurasian, Iberian and African plates during the late Eocene to the Miocene. The main trend of its contractional structures is NW-SE, but E-W, NE-SW and N-S-trending structures are also present....

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Bibliografski detalji
Izdano u:Geologica Acta: an international earth science journal
Glavni autor: Joan Guimerà
Format: Artigo
Jezik:Inglês
Izdano: Universitat de Barcelona 2018
Teme:
Online pristup:https://www.redalyc.org/articulo.oa?id=50559030006
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