RT Journal Article
T1 El cabalgamiento de Valdesotos: consecuencias de la acomodación del acortamiento cenozoico en el zócalo del Sistema Central
A1 Olaiz Campos, Antonio José
A1 Vicente Muñoz, Gerardo De
A1 Vegas Martínez, Ramón
A1 González Casado, José Manuel
A1 Muñoz Martín, Alfonso
A1 Álvarez, J.
AB We describe and study structural evidences concerning to Alpine tectonics at NE sector o f the Spanish Central System (SCS). In Valdesotos area, the Hercynian basement is uplifted over Mesozoic sediments, throughout a main SW verging thrust. Fault population analysis and geological mapping has been used to look at the relation between structures in the basement and in the cover. As a consequence of accommodation of strains in the basement, kink folds are developed, such as secondary thrust and folds in the tegument. All these meso- and macrostructures seem to answer to a shortening in agreement with the Cenozoic deformation.
PB Sociedad Geológica de España.
SN 1576-5172
YR 2004
FD 2004
LK https://hdl.handle.net/20.500.14352/52548
UL https://hdl.handle.net/20.500.14352/52548
LA spa
DS Docta Complutense
RD 15 abr 2025