Rift-related volcanism predating the birth of the Rheic Ocean

Two very different periods of magma emplacement in the crust of the Ossa-Morena zone (early and main events) in SW Iberia have been previously interpreted to record a Cambrian/Early Ordovician rifting event that is thought to have culminated in the opening of the Rheic Ocean during the Early Ordovic...

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Detalhes bibliográficos
Autor principal: Sanchez-Garcia, Teresa (author)
Outros Autores: Bellido, Felix (author), Pereira, M. Francisco (author), Chichorro, Martim (author), Quesada, Cecilio (author), Pin, Christian (author), Silva, Jose B. (author)
Formato: article
Idioma:eng
Publicado em: 2011
Assuntos:
Rift magmatism
Cambrian–Ordovician
Geochemistry
Rheic Ocean
Ossa-Morena zone
Sm–Nd isotopes
Texto completo:http://hdl.handle.net/10174/2979
País:Portugal
Oai:oai:dspace.uevora.pt:10174/2979

Texto Completo

http://hdl.handle.net/10174/2979

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