%0 Journal Article
%A Rodríguez Pascua, M.A.
%A Vicente Muñoz, Gerardo de
%A González Casado, J.M.
%T Cinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)
%D 1994
%@ 0213-4497
%U https://hdl.handle.net/20.500.14352/59881
%X The geological macrostructure of Alto Tajo is defined by several N1500E dextral strike-slip faults with related secundary structures. The former set of faults together with others N-S sinistral strike-slip faults delimited areas in transtension and transpession. Four tectonic phases have been detected by means of microstructural analysis: N600E compression; N1500E compression (the main deformation phase). N-S compression, without important structures asociated and a last episode of radial extension.
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