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dc.contributor.authorCendrero, A.
dc.contributor.authorDíaz de Terán, J. R.
dc.contributor.authorMoñino, M.
dc.date.accessioned2020-06-26T09:25:15Z
dc.date.available2020-06-26T09:25:15Z
dc.date.issued1988
dc.identifier.urihttp://hdl.handle.net/10272/18391
dc.description.abstractEvidence of faulting with displacements of several meters in a fluvial terrace 20 m above the present river level has been found in Polanco, near Santander. The site is located nead a diapir of Triassic clays and salts. This shows that there has been deformation in the area during late Quaternary times, perhaps only in relation to diapir emplacementes_ES
dc.language.isospaes_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherFluvial terraceses_ES
dc.subject.otherNeotectonicses_ES
dc.titleDeformación de terrazas fluviales recientes en la franja costera cantábricaes_ES
dc.typeinfo:eu-repo/semantics/articlees_ES
dc.rights.accessRightsinfo:eu-repo/semantics/openAccesses_ES


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Atribución-NoComercial-SinDerivadas 3.0 España
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