Early Cambrian granitoids of North Gondwana margin in the transition from a convergent setting to intra-continental rifting (Ossa-Morena Zone, SW Iberia).

Two distinct Cambrian magmatic pulses are recognized in the Ossa-Morena Zone (SW Iberia): an early rift-(ER) and a main rift-related event. This Cambrian magmatism is related to intra-continental rifting of North Gondwana that is thought to have culminated in the opening of the Rheic Ocean in Lower...

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Detalhes bibliográficos
Autor principal: Sanchez-Garcia, T (author)
Outros Autores: Pereira, M Francisco (author), Bellido, F (author), Chichorro, M (author), Silva, JB (author), Valverde-Vaquero, P (author), Pin, Ch (author), Sola, AR (author)
Formato: article
Idioma:eng
Publicado em: 2014
Assuntos:
Cambrian magmatism
U-Pb geochronology
isotopes
Iberia
Texto completo:http://hdl.handle.net/10174/9465
País:Portugal
Oai:oai:dspace.uevora.pt:10174/9465

Texto Completo

http://hdl.handle.net/10174/9465

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