Early Carboniferous synorogenic basins evolution of the Ossa-Morena and

The stratigraphic record of the Early Carboniferous in Iberia reveals that synorogenic deposition was important and occurred simultaneously in basins influenced by extension and contraction with gravitational instability. In NW Iberia (Galicia – Trás-os-Montes Zone) contraction was dominant and the...

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Bibliographic Details
Main Author: Pereira, M Francisco (author)
Other Authors: Dias da Silva, Icaro F (author), Gama, Cristina (author), Castro, Antonio (author), Fernandez, Carlos (author)
Format: lecture
Language:eng
Published: 2017
Subjects:
Synorogenic deposition
Magmatism
Contraction and extension
Early Carboniferous
Variscan orogeny
Online Access:http://hdl.handle.net/10174/20495
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/20495

Internet

http://hdl.handle.net/10174/20495

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