The Significance of Changes of Source Areas During Carboniferous Turbiditic Deposition (Southwestern Iberia)

U–Pb dating of detrital zircons from the Carboniferous turbidites of southwestern Iberia (the Cabrela, Mértola, Mira, and Brejeira formations) shows that synorogenic sedimentation during the Carboniferous was marked by significant variations in the source areas, involving the denudation of different...

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Detalhes bibliográficos
Autor principal: Pereira, Manuel Francisco (author)
Outros Autores: Chichorro, Martim (author), Gutierrez-Alonso, G. (author), Vilallonga, Filipa (author), Drost, K. (author), Ribeiro, Carlos (author), Silva, J.B. (author), Albardeiro, Luis (author), Hofmann, M. (author), Linnemann, U. (author)
Formato: lecture
Idioma:por
Publicado em: 2015
Assuntos:
U-Pb geochronology
South Portuguese Zone
Ossa-Morena Zone
Variscan orogeny
Pangea
Texto completo:http://hdl.handle.net/10174/13458
País:Portugal
Oai:oai:dspace.uevora.pt:10174/13458

Texto Completo

http://hdl.handle.net/10174/13458

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