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dc.contributor.authorCendrero, A.
dc.contributor.authorDíaz de Terán, J. R.
dc.contributor.authorMoñino, M.
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.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherFluvial terraceses_ES
dc.titleDeformación de terrazas fluviales recientes en la franja costera cantábricaes_ES

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Atribución-NoComercial-SinDerivadas 3.0 España
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