Transected folds with opposite patterns in Terena Formation (Ossa Morena Zone, Portugal): anomalous structures resulting from sedimentary basin anisotropies

Abstract The Terena Formation is located in the central part of the Ossa-Morena Zone (OMZ) and outcrops in the core of a latter (D3) first order syncline. This Formation is a Lower Devonian flysch and shows an unusual “Z” shape, with a central sector trending nearly N-S, and the tips trending NW-SE....

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Bibliographic Details
Main Author: Rocha, Rodrigo Camargo (author)
Other Authors: Araújo, António Alexandre (author), Borrego, José Santos (author), Fonseca, Paulo Emanuel (author)
Format: article
Language:eng
Published: 2010
Subjects:
Transected folds
Variscan
Iberian Peninsula
Sintectonic flysch
Terena Syncline
Ossa Morena Zone
Online Access:http://hdl.handle.net/10174/2217
Country:Portugal
Oai:oai:dspace.uevora.pt:10174/2217

Internet

http://hdl.handle.net/10174/2217

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