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Neotectonic processes in marine terrace sediments near Canero (Western Asturias)

dc.contributor.authorGutiérrez Claverol, M.
dc.contributor.authorLópez Fernández, C.
dc.contributor.authorAlonso, J. L.
dc.date.accessioned2014-07-25T09:56:25Z
dc.date.available2014-07-25T09:56:25Z
dc.date.issued2006
dc.identifier.urihttp://hdl.handle.net/10272/8625
dc.description.abstractThe Pleistocene sediments deposited on the emerged marine abrasion platform near Canero village (Valdés, Asturias) are truncated by reverse faults which are parallel to basement bedding. These structures imply a neotectonic activity with a NW-SE maximum compressive stress, consistent with recent fault population analysis and current seismicity studies. The described deformation corresponds to a reactivation of folds in the Palaeozoic basement through a flexural slip mechanism, with the subsequent accommodation of the unconformable Pleistocene coveren_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.otherNeotectonicsen_US
dc.subject.otherSeismicityen_US
dc.subject.otherMarine terraceen_US
dc.subject.otherFlexural-slip faultsen_US
dc.subject.otherPleistoceneen_US
dc.titleProcesos neotectónicos en los depósitos de rasa de la zona de Canero (Occidente de Asturias)en_US
dc.titleNeotectonic processes in marine terrace sediments near Canero (Western Asturias)eng
dc.typeinfo:eu-repo/semantics/articleen_US
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess


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