RT Journal Article
T1 Cinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)
T2 Kinematic and dynamic array of the alpine deformations in alto Tajo are a (Guadalajara)
A1 Rodríguez Pascua, M.A.
A1 Vicente Muñoz, Gerardo De
A1 González Casado, J.M.
AB 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.
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/20.500.14352/59881
UL https://hdl.handle.net/20.500.14352/59881
LA spa
DS Docta Complutense
RD 1 sept 2024