RT Journal Article
T1 Reconocimiento geoeléctrico de paleovalles en la depresión terciaria de Ciudad Rodrigo
T1 Geoelectrical recognition of paleo-valleys in Ciudad Rodrigo Tertiary depression
A1 Corrochano, A.
A1 Andrés, M. F.
A1 Barba, Pedro
A1 Curiel, N.
A1 Armenteros, Ildefonso
AB The 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 observations
PB Sociedad Geológica de España
YR 2000
FD 2000
LK http://hdl.handle.net/10272/9830
UL http://hdl.handle.net/10272/9830
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026