Reconocimiento geoeléctrico de paleovalles en la depresión terciaria de Ciudad Rodrigo

dc.contributor.authorCorrochano, A.
dc.contributor.authorAndrés, M. F.
dc.contributor.authorBarba, Pedro
dc.contributor.authorCuriel, N.
dc.contributor.authorArmenteros, Ildefonso
dc.date.accessioned2015-02-09T10:18:40Z
dc.date.available2015-02-09T10:18:40Z
dc.date.issued2000
dc.description.abstractThe V.E.S. (vertical electrical sounding) study undertaken in the Ciudad Rodrigo Craben unravels the structure and the lithology of the graben infill. The basement resistivity values (200-350 Qm) indicate the presence of NW-SE oriented paleovalleys which were responsible for the tertiary drainage. The resistivity values of the tertiary rocks show the presence of sandstones and conglomerates (40-70 Qm), sand and clay (20-30 ?m) and claystone (10-18 ?m). Each of these groups can be correlated to Paleogene and Neogene rocks according to surface observationsen_US
dc.identifier.urihttp://hdl.handle.net/10272/9830
dc.language.isospaen_US
dc.publisherSociedad Geológica de Españaen_US
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.rights.accessRightsopen accessen_US
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/3.0/es/*
dc.subject.otherGeophysical prospegtingen_US
dc.subject.otherResistivityen_US
dc.subject.otherCiudad Rodrigo Depressionen_US
dc.titleReconocimiento geoeléctrico de paleovalles en la depresión terciaria de Ciudad Rodrigoen_US
dc.titleGeoelectrical recognition of paleo-valleys in Ciudad Rodrigo Tertiary depressioneng
dc.typejournal articleen_US
dspace.entity.typePublication

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