%0 Journal Article
%A Giner Robles, Jorge Luis
%A Vicente Muñoz, Gerardo de
%A González Casado, J.M.
%T Neotectónica del borde oriental de la cuenca de Madrid
%D 1994
%@ 0213-4497
%U https://hdl.handle.net/20.500.14352/59883
%X 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).
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