Corrochano, A.Andrés, M. F.Barba, PedroCuriel, N.Armenteros, Ildefonso2015-02-092015-02-092000http://hdl.handle.net/10272/9830The 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 observationsspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Geophysical prospegtingResistivityCiudad Rodrigo DepressionReconocimiento geoeléctrico de paleovalles en la depresión terciaria de Ciudad RodrigoGeoelectrical recognition of paleo-valleys in Ciudad Rodrigo Tertiary depressionjournal articleopen access