Las deformaciones hercinianas tardías en la región de Santa María la Real de Nieva (Sistema Central Español)
The precambrian and paleozoic materials of Santa María la Real de Nieva outcrop has been affected by two Hercynian shear systems which developed after the main deformation phases and the intrusion of the granite rocks. The first shear system is composed of subvertical, dipping northwards, senestral...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1988 |
| País: | España |
| Recursos: | Universidad de Huelva (UHU) |
| Repositorio: | Arias Montano. Repositorio Institucional de la Universidad de Huelva |
| Idioma: | español |
| OAI Identifier: | oai:ariasmontano.uhu.es:10272/18377 |
| Acesso em linha: | http://hdl.handle.net/10272/18377 |
| Access Level: | acceso abierto |
| Palavra-chave: | Structural geology Hercynian Orogeny Spanish Central System |
| Resumo: | The precambrian and paleozoic materials of Santa María la Real de Nieva outcrop has been affected by two Hercynian shear systems which developed after the main deformation phases and the intrusion of the granite rocks. The first shear system is composed of subvertical, dipping northwards, senestral wrench faults trending ENE-WSW. The second is a Iow-angle extensional system with the hanging wall descending westwards |
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