The Cadomian Orogeny and the opening of the Rheic Ocean: The diacrony of

Cadomian orogenic processes and their continuum to the opening of the Rheic Ocean were modeled by making use of new LA-ICP-MS U–Pb ages from detrital zircons of sedimentary rocks of Late Neoproterozoic (Ediacaran) and Cambro-Ordovician sediments of the Ossa-Morena Zone (Iberian Massif) compared with...

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Detalhes bibliográficos
Autor principal: Linnemann, Ulf (author)
Outros Autores: Pereira, M. Francisco (author), Jeffries, Teresa (author), Drost, Kerstin (author), Gerdes, Axel (author)
Formato: article
Idioma:eng
Publicado em: 2011
Assuntos:
Cadomian Orogeny
Rheic Ocean
West African Craton
Gondwana
Saxo-Thuringain Zone
Ossa-Morena Zone
Neoproterozoic
Cambrian
Ordovician
Texto completo:http://hdl.handle.net/10174/2966
País:Portugal
Oai:oai:dspace.uevora.pt:10174/2966

Texto Completo

http://hdl.handle.net/10174/2966

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