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dc.contributor.authorFernández García, J.
dc.date.accessioned2016-09-21T12:04:19Z
dc.date.available2016-09-21T12:04:19Z
dc.date.issued1996
dc.identifier.urihttp://hdl.handle.net/10272/12670
dc.description.abstractThe Viveiro fault is a ductile normal fault of Hercynian age which separates two distinct lithological units metamorphic evolution and tectonic styles. The foot wall in the east forms the Lugo dome, made with diferent Cambrian and pre-Cambrian metasediments with dominant flat-lying foliation and E-W trending stretching lineation. The hanging-wall in the west consist of a domain of tight upright folds with associated west dipping dominant foliation. An upright synform with a core of Silurian rocks is pinched between the Viveiro fault and the westerly located complex Olio de Sapo antiformen_US
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherViveiro faulen_US
dc.subject.otherSynformen_US
dc.subject.otherPincheden_US
dc.titleSobre el origen de la falla de Viveiro y su evolución respecto al macizo hercinico (Prov. De Lugo)en_US
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccessen_US


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