Sobre la estructura del Antiforme de El Cardoso y el Sinforme de Majaelrayo y su relación con la Falla de Berzosa
The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the third hercynian deformation phase (F) and are cross-cut by the Berzosa Fault, a normal accident with a dextral wrench component. The ductile shear zone that outcrops in the core the El Cardoso Antiform...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1988 |
| 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:10272/18403 |
| Acceso en línea: | http://hdl.handle.net/10272/18403 |
| Access Level: | acceso abierto |
| Palabra clave: | Geología estructural Orógeno Herciniano Sierra de Guadarrama Structural geology Hercynian Orogeny |
| Sumario: | The El Cardoso Antiform and the Majaelrayo Synform are structures which were generated during the third hercynian deformation phase (F) and are cross-cut by the Berzosa Fault, a normal accident with a dextral wrench component. The ductile shear zone that outcrops in the core the El Cardoso Antiform can be related to that which exists west of the Berzosa Fault and also to that which affects the overturned limb of the Hiendelaencina Anticline |
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