2026-04-21T04:46:22Zhttps://riubu.ubu.es/oai/requestoai:riubu.ubu.es:10259/90272024-04-25T00:05:16Zcom_10259_9025com_10259_5086com_10259_2604com_10259.4_2560col_10259_9026col_10259.4_2561
Bógalo Román, Mª Felicidad
Osete López, María Luisa
Ancochea Soto, Eumenio
Villalaín Santamaria, Juan José
2024-04-24T09:53:13Z
2024-04-24T09:53:13Z
1993
0213-683X
http://hdl.handle.net/10259/9027
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.
Este trabajo ha sido financiado por el proyecto de la DGICYT PB89-0141.
application/pdf
spa
Sociedad Geológica de España
Geogaceta. 1993, n. 15, p. 109-112
https://sociedadgeologica.org/publicaciones/geogaceta/geogaceta-15-1993/
Paleomagnetism
Volcanism
Iberian Plate
Campos de Calatrava
Física
Magnetismo
Geología
Physics
Magnetism
Geology
Estudio paleomagnético del volcanismo de Campos de Calatrava
Paleomagnetic study of the volcanism in Campos de Calatrava
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
info:eu-repo/semantics/openAccess
Geogaceta
15
109
112