Crustal growth and deformational processes in the northern Gondwanan margin: constraints from the Évora Massif (Ossa-Morena zone, southwest Iberia, Portugal)

The aim of this article is to present a compilation of available information on the Évora Massif based on structural mapping, whole-rock geochemistry, recognition of metamorphic mineral assemblages, and geothermobarometry. In our view, transcurrent movements responsible for strong orogen-parallel st...

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Bibliographic Details
Main Author: Pereira, M. F. (author)
Other Authors: Silva, J. B. (author), Chichorro, M. (author), Moita, P. (author), Santos, J. F. (author), Apraiz, A. (author), Ribeiro, C. (author)
Format: article
Language:eng
Published: 1000
Subjects:
Early Paleozoic rifting
Variscan orogeny
Transcurrent tctonics
High-grade terranes
Local transtension
Online Access:http://hdl.handle.net/10773/13841
Country:Portugal
Oai:oai:ria.ua.pt:10773/13841

Internet

http://hdl.handle.net/10773/13841

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