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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Bibliographic Details
Main Author: Quesada, Cecilio (author)
Other Authors: 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)
Format: bookPart
Language:por
Published: 2020
Subjects:
Ophiolites
Ossa-Morena Zone
Online Access:http://hdl.handle.net/10174/26471
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/26471

Internet

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

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