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Recumbent folding in Serra do Galiñeiro (Pontevedra, NW Spain)

dc.contributor.authorDíez Fernández, Rubén
dc.contributor.authorMartínez Catalán, José R.
dc.contributor.authorAbati, J.
dc.date.accessioned2014-07-17T16:53:17Z
dc.date.available2014-07-17T16:53:17Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8587
dc.description.abstractThree main deformation phases (D1, D2 and D3) have been identified in the Serra do Galiñeiro using macro and microstructural analysis. The geometric characterization of those showing macrostructural elements (D2 and D3), has been made with the down-plunge method, for the folds related to each phase. In order to apply this technique, the fold axis orientation has been calculated from the structural data collected. The results of this research prove the existence of recumbent folds in the southern part of the Malpica-Tui Unit, and the presence of a stretching lineation related to the main foliation and the recumbent folds, and clearly oblique to their axesen_US
dc.language.isospaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/
dc.subject.otherRecumbent foldingen_US
dc.subject.otherAllochthonous complexesen_US
dc.subject.otherNW Iberiaen_US
dc.titlePlegamiento recumbente en la Serra do Galiñeiro (Pontevedra, NO España)en_US
dc.titleRecumbent folding in Serra do Galiñeiro (Pontevedra, NW Spain)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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