Provenance of Cambro-Ordovician siliciclastic rocks of the SW Iberia: insights to the evolution of North Gondwana margin.

This study makes a comparison between the populations of detrital zircon of the Cambrian sandstones from the Ossa-Morena Zone (OMZ) and the Ordovician quartzites from the southern domains of the Central Iberian Zone (S-CIZ) in order to identify the sources during development of North Gondwana basins...

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Detalhes bibliográficos
Autor principal: Solá, Rita (author)
Outros Autores: Chichorro, Martim (author), Pereira, Manuel Francisco (author), Hofmann, M. (author), Linnemann, U. (author), Gerdes, A. (author), Medina, Jorge (author), Lopes, Luís (author)
Formato: lecture
Idioma:por
Publicado em: 2014
Assuntos:
SW Iberia
Cambro-Ordovician
rifting
zircon
Texto completo:http://hdl.handle.net/10174/10372
País:Portugal
Oai:oai:dspace.uevora.pt:10174/10372

Texto Completo

http://hdl.handle.net/10174/10372

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