Tracing the Cadomian magmatism with detrital/inherited zircon ages by in-situ U–Pb SHRIMP geochronology (Ossa-Morena Zone, SW Iberian Massif),

U–Pb SHRIMP geochronology on zircon extracted from a granite, a sandstone and a quartzite of the SW Iberian Massif (Ossa-Morena Zone), was used in order to investigate the contribution of Late Neoproterozoic (Cadomian) tectonothermal history to the crustal growth of northern Gondwana. The analysed C...

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Detalhes bibliográficos
Autor principal: Pereira, M. Francisco (author)
Outros Autores: Chichorro, Martim (author), Solá, A.M. Rita (author), Silva, Jose B. (author), Sánchez-Garcia, Teresa (author), Bellido, Felix (author)
Formato: article
Idioma:eng
Publicado em: 2011
Assuntos:
Detrital/inherited zircon ages
Cadomian magmatic arc
Ediacaran
Cambrian
Northern Gondwana margin
Texto completo:http://hdl.handle.net/10174/2982
País:Portugal
Oai:oai:dspace.uevora.pt:10174/2982

Texto Completo

http://hdl.handle.net/10174/2982

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