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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Detalhes bibliográficos
Autor principal: Pereira, M Francisco (author)
Outros Autores: Dias da Silva, Icaro F (author), Gama, Cristina (author), Castro, Antonio (author), Fernandez, Carlos (author)
Formato: lecture
Idioma:eng
Publicado em: 2017
Assuntos:
Synorogenic deposition
Magmatism
Contraction and extension
Early Carboniferous
Variscan orogeny
Texto completo:http://hdl.handle.net/10174/20495
País:Portugal
Oai:oai:dspace.uevora.pt:10174/20495

Texto Completo

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

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