Estudio paleomagnético del volcanismo de Campos de Calatrava
A first systematic paleomagnetic study has been carried out in the upper Miocene-Pliocene volcanism ofthe Campos de Calatrava region. 18 localities have been sampled and 14 of them yielded useful paleomagnetic results. A Pliocene paleomagnetic pole has been obtained for the Iberian Plate (Lat.= 82.1...
| Autores: | , , , |
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| Tipo de recurso: | artículo |
| Fecha de publicación: | 1994 |
| 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:10272/13991 |
| Acceso en línea: | http://hdl.handle.net/10272/13991 |
| Access Level: | acceso abierto |
| Palabra clave: | Paleomagnetism Campos de Calatrava Volcanism Iberian Plate |
| Sumario: | A first systematic paleomagnetic study has been carried out in the upper Miocene-Pliocene volcanism ofthe Campos de Calatrava region. 18 localities have been sampled and 14 of them yielded useful paleomagnetic results. A Pliocene paleomagnetic pole has been obtained for the Iberian Plate (Lat.= 82.1°N, Long.= 171.6°E, Ags= 6.9). On the basis ofthe magnetic polarity results a zoning of the volcanism may be recognized which could be explained by a NE-ward migration of the volcanism in this region |
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