SW Iberia Variscan Suture Zone: Oceanic Affinity Units

The geology of SW Iberia records a sequence of geologic events from the Cambrian-Early Ordovician rifting and subsequent passive margin development along the southern flank of the Rheic Ocean, to onset of oblique (sinistral) subduction in the Devonian, followed by oblique terrane accretion, ocean cl...

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Detalhes bibliográficos
Autor principal: Quesada, Cecilio (author)
Outros Autores: Braid, J. A. (author), Murphy, J. B. (author), Fernandes, Paulo (author), Ferreira, Pedro (author), Oliveira, José Tomás (author), Jorge, Raul (author), Matos, José Xavier (author), Pedro, Jorge (author), Pereira, Zélia (author)
Formato: bookPart
Idioma:por
Publicado em: 2020
Assuntos:
Ophiolites
Ossa-Morena Zone
Texto completo:http://hdl.handle.net/10174/26471
País:Portugal
Oai:oai:dspace.uevora.pt:10174/26471

Texto Completo

http://hdl.handle.net/10174/26471

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