Estudio paleomagnético del volcanismo de Campos de Calatrava
A first systematic paleomagnetic study has been carried out in the upper Miocene-Pliocene volcanism of the 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 |
| Estado: | Versión publicada |
| Fecha de publicación: | 1993 |
| País: | España |
| Institución: | Universidad de Burgos (UBU) |
| Repositorio: | Repositorio Institucional de la Universidad de Burgos (RIUBU) |
| OAI Identifier: | oai:riubu.ubu.es:10259/9027 |
| Acceso en línea: | http://hdl.handle.net/10259/9027 |
| Access Level: | acceso abierto |
| Palabra clave: | Paleomagnetism Volcanism Iberian Plate Campos de Calatrava Física Magnetismo Geología Physics Magnetism Geology |
| Sumario: | A first systematic paleomagnetic study has been carried out in the upper Miocene-Pliocene volcanism of the 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.=82.1ºN, Long.= 171.6ºE, A95=6.9). On the basis of the 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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