Variscan structural evolution of the western High Atlas and the Hauouz plain (Morocco)

The Variscan belt is one of the major geological features of Morocco. Based on the paleogeography of the Paleozoic formations and related tectonometamorphic evolution, different domains have been proposed for this segment of the orogen. The Western High Atlas is one of such domains, which is usually...

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Bibliographic Details
Main Author: Dias, Rui (author)
Other Authors: Hadani, Mohamed (author), Leal Machado, Isabel (author), Adane, Naima (author), Hendaq, Youssef (author), Madih, Khadija (author), Matos, Catarina (author)
Format: article
Language:por
Published: 2012
Subjects:
Morocco
Variscan orogeny
Western High Atlas
Haouz plain
Dextral oblique collision
Online Access:http://hdl.handle.net/10174/4398
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/4398

Internet

http://hdl.handle.net/10174/4398

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