Tardi-Variscan Deformation in Ibero-Moroccan Sector; Implications on Pangeia Assemblage
The tardi-Variscan structures in the Ibero-Moroccan domain show a brittle-ductile behaviour, overlapping the earlier main ductile stages, developed in the same orogenic process. The interaction between tectonic thickening, erosion and isostasy during the progressive colisional stages of the Variscan...
Main Author: | |
---|---|
Other Authors: | , , , |
Format: | lecture |
Language: | eng |
Published: |
2014
|
Subjects: | |
Online Access: | http://hdl.handle.net/10174/10227 |
Country: | Portugal |
Oai: | oai:dspace.uevora.pt:10174/10227 |