«La Falla de Urriza (Pirineo Occidental): Neotectónica en materiales del cretácico superior del norte de Navarra»
In the north of Navarra (Western Pyrenees), subvertical folds with characteristic density of diaclases in the hinge zone outcrop in upper cretaceous beds. Its genesis has been associated to a sinistral wrench affecting quaternarian terraces. So, a neotectonic genesis can be assumed to explain the fo...
| Autores: | , , |
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| Formato: | artículo |
| Fecha de publicación: | 1990 |
| 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:10272/18184 |
| Acesso em linha: | http://hdl.handle.net/10272/18184 |
| Access Level: | acceso abierto |
| Palavra-chave: | Neotectonics Folds Upper cretaceous Navarra Western Pyrenees |
| Resumo: | In the north of Navarra (Western Pyrenees), subvertical folds with characteristic density of diaclases in the hinge zone outcrop in upper cretaceous beds. Its genesis has been associated to a sinistral wrench affecting quaternarian terraces. So, a neotectonic genesis can be assumed to explain the folds developed in cretaceous materials |
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