RT Journal Article
T1 Neotectónica del borde oriental de la cuenca de Madrid
T2 Neotectonics of the eastern border of the Madrid basin
A1 Giner Robles, Jorge Luis
A1 Vicente Muñoz, Gerardo de
A1 González Casado, J.M.
AB An analysis of the neotectonic activity and the current stress state of the eastern border of Madrid Basin has been carried ont using structural-methods (fault population analysis), as well as seismological methods. Two stress tensors have been established:- Tensor 1: with a N1500E shortening trend, characterized mainly by strikeslip faults. This tensor corresponds to the «Guadarrama» stress field (Capote et al., 1990), wihch causes the Central System structure; dated middle Aragonian-lower Pleistocene in the eastern border ofMadrid Basin (Muñoz Martín, 1993).- Tensor 2: dated post-lower Pleistocene, with a N150° E extension trend, characterized basically by normal faults.Actual stress tensor deduced focal mechanisms by the seismological method is compatible with the paleostress field deduced for the middle-lower Pleistocene(tensor 2).
PB Seminario de Estudos Galegos. Area de Xeoloxía e Minería ;  Instituto Universitario de Xeoloxía "Isidro Parga Pondal"
SN 0213-4497
YR 1994
FD 1994
LK https://hdl.handle.net/20.500.14352/59883
UL https://hdl.handle.net/20.500.14352/59883
LA spa
NO España. Dirección General de Investigación Científica y Técnica
DS Docta Complutense
RD 2 ago 2024