El pliegue sinsedimentario de Hinojares (sector de Pozo Alcón-Tíscar, provincia de Jaén, zona externa bética)
In the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the recent glacis, Pleistocene in age, shows two flexions parallel to the fold hinge...
| Autores: | , , , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 2006 |
| 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:10272/8466 |
| Acceso en línea: | http://hdl.handle.net/10272/8466 |
| Access Level: | acceso abierto |
| Palabra clave: | Growth syncline Neotectonics Active Tectonics Guadix-Baza basin Rodent tooth |
| Sumario: | In the proximities of Hinojares (northern border of the Guadix-Baza basin), there is a growth syncline, formed in Plio-Quaternary sediments, showing progressive unconformities in its limbs. At its ESE prolongation, the recent glacis, Pleistocene in age, shows two flexions parallel to the fold hinge and limbs. This fold has been probably controlled by the Tiscar fault and formed within a NNE-SSW compressive setting |
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