New data on the late Famennian miospore assemblage of the Cercal Anticline (westernmost Iberian Pyrite Belt area), Portugal

The Cercal Anticline (CA) is located in the westernmost region of the Iberian Pyrite Belt (IPB). The exposed stratigraphic sequence includes, in ascending order, the Volcano-Sedimentary Complex (VSC) followed by the Xistos das Abertas Fm, which passes gradually to the flysch sequence of the Mira For...

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Detalhes bibliográficos
Autor principal: Pereira, Zélia (author)
Outros Autores: Matos, João Xavier (author), Fernandes, Paulo (author), Oliveira, José Tomás (author)
Formato: conferenceObject
Idioma:eng
Publicado em: 2014
Assuntos:
Palinologia
Miosporos
Fameniano
Anticlinal do Cercal (Portugal)
Faixa Piritosa Ibérica
Texto completo:http://hdl.handle.net/10400.1/5074
País:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/5074
Descrição
Resumo:The Cercal Anticline (CA) is located in the westernmost region of the Iberian Pyrite Belt (IPB). The exposed stratigraphic sequence includes, in ascending order, the Volcano-Sedimentary Complex (VSC) followed by the Xistos das Abertas Fm, which passes gradually to the flysch sequence of the Mira Formation (Carvalho, 1976).

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