Cinemática y dinámica de las deformaciones en la zona del alto Tajo (Guadalajara)
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 detect...
| Autores: | , , |
|---|---|
| Tipo de recurso: | artículo |
| Fecha de publicación: | 1994 |
| País: | España |
| Institución: | Universidad Complutense de Madrid (UCM) |
| Repositorio: | Docta Complutense |
| Idioma: | español |
| OAI Identifier: | oai:docta.ucm.es:20.500.14352/59881 |
| Acceso en línea: | https://hdl.handle.net/20.500.14352/59881 |
| Access Level: | acceso abierto |
| Palabra clave: | 551.24(460.281) (460.281)551.24 Fallas (Geología) España-Guadalajara Strike-slip Faults Flower structures Fault population analysis Cataclastic rocks Tertiary basin of Zaorejas Geodinámica 2507 Geofísica |
| Sumario: | 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. |
|---|