Rodríguez Pascua, M.A.Vicente Muñoz, Gerardo DeGonzález Casado, J.M.2023-06-202023-06-2019940213-4497https://hdl.handle.net/20.500.14352/59881The 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.spaCinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)Kinematic and dynamic array of the alpine deformations in alto Tajo are a (Guadalajara)journal articlehttp://www.iux.es/?page=5&serie=1open access551.24(460.281)(460.281)551.24Fallas (Geología)España-GuadalajaraStrike-slipFaultsFlower structuresFault population analysisCataclastic rocksTertiary basin of ZaorejasGeodinámica2507 Geofísica