Geodynamic evolution of Ossa-Morena Zone in a SW Iberian context during the Variscan cycle

Ossa-Morena Zone (OMZ) is crucial to understanding the geodynamic evolution of the Variscan cycle in SW Iberia. We review previous data, from Early to Late Paleozoic. The early Cambrian (conglomeratic and felsic metavolcanic units) lies unconformably upon Neoproterozoic formations and shows a carbon...

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Detalhes bibliográficos
Autor principal: Moreira, Noel (author)
Outros Autores: Araújo, Alexandre (author), Pedro, Jorge (author), Dias, Rui (author)
Formato: lecture
Idioma:eng
Publicado em: 2015
Assuntos:
Variscan
Iberia
tectono-metamorphic
Rheic
Texto completo:http://hdl.handle.net/10174/13464
País:Portugal
Oai:oai:dspace.uevora.pt:10174/13464

Texto Completo

http://hdl.handle.net/10174/13464

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