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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Bibliographic Details
Main Author: Pereira, Zélia (author)
Other Authors: Matos, João Xavier (author), Fernandes, Paulo (author), Oliveira, José Tomás (author)
Format: conferenceObject
Language:eng
Published: 2014
Subjects:
Palinologia
Miosporos
Fameniano
Anticlinal do Cercal (Portugal)
Faixa Piritosa Ibérica
Online Access:http://hdl.handle.net/10400.1/5074
Country:Portugal
Oai:oai:sapientia.ualg.pt:10400.1/5074
Description
Summary: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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