Sedimentación marina somera en el devónico del anticlinorio de Puebla de Guzmán, Faja Pirítica Ibérica
The sedimentary nature of the rocks outcroping near the Virgen de la Peña hermitage suggests a shallow marine sedimentation, with a main influence of swell, almost for a part of the PQ Group of the Iberian Pyrite Belt in the Puebla de Guzman Anticline
| 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:10272/18198 |
| Acesso em linha: | http://hdl.handle.net/10272/18198 |
| Access Level: | acceso abierto |
| Palavra-chave: | PQ Group Devonian Iberian Pyrite Belt Huelva |
| Resumo: | The sedimentary nature of the rocks outcroping near the Virgen de la Peña hermitage suggests a shallow marine sedimentation, with a main influence of swell, almost for a part of the PQ Group of the Iberian Pyrite Belt in the Puebla de Guzman Anticline |
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