2026-04-21T04:45:30Zhttps://riubu.ubu.es/oai/request

oai: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 Paleomagnetism Volcanism Iberian Plate 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.=82.1ºN, 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. 2024-04-24 2024-04-24 1993 info:eu-repo/semantics/article 0213-683X http://hdl.handle.net/10259/9027 spa Geogaceta. 1993, n. 15, p. 109-112 https://sociedadgeologica.org/publicaciones/geogaceta/geogaceta-15-1993/ info:eu-repo/semantics/openAccess Sociedad Geológica de España