Características estructurales y geométricas de la falla de desgarre de Lorca-Alhama
The Lorca-Alhama fault is one of the more tectonic and seismically active sinistraI strike-slip fault of the eastern Betics. Its complex structural pattern records simultaneous development of ex- tensional and contractional features, which can be explained by a simple sinistral shear model. Spatial...
| Autores: | , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1992 |
| País: | España |
| Institución: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/16323 |
| Acceso en línea: | http://hdl.handle.net/10272/16323 |
| Access Level: | acceso abierto |
| Palabra clave: | Structural pattern Geometry Simple shear Fault segmentation Lorca-Alhama fault Eastern Betics |
| Sumario: | The Lorca-Alhama fault is one of the more tectonic and seismically active sinistraI strike-slip fault of the eastern Betics. Its complex structural pattern records simultaneous development of ex- tensional and contractional features, which can be explained by a simple sinistral shear model. Spatial coincidence of structural and geometric diagnostic features of segment boundaries along the strike of the fault, are reflecting the segmented nature of this tectonic accident |
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