Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/3034
Full metadata record
DC FieldValueLanguage
dc.creatorLópez Ruiz, J.-
dc.creatorRodríguez Badiola, Eduardo-
dc.creatorCebriá Gómez, J. M.-
dc.date2008-02-24T13:20:36Z-
dc.date2008-02-24T13:20:36Z-
dc.date1986-12-
dc.date.accessioned2017-01-31T01:00:20Z-
dc.date.available2017-01-31T01:00:20Z-
dc.identifierGeogaceta, Nº1, 28-31-
dc.identifier0213-683X-
dc.identifierhttp://hdl.handle.net/10261/3034-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/3034-
dc.descriptionCompositional trends and trace elements abundance in leucite-basanites, nepheline-basanites and olivíne basalts from la Garrotxa (NE Spain region), suggest that the parental magma were originated from an homogeneous lherzolite source, strongly enriched in incompatible elements (between x15-x4 the chondritic values for the highly incompatible elements and between x5-x2 for the moderately incompatible), in which neither kaersutite, phlogopite or apatite remained as residual phases. The leucite-basanite magmas were derived by lower degrees of melting (7-10%) than the basanite s,s. and the olivine basalt magmas (13-15%). Except some primary leucite-basanites, the lavas from La Garrotxa underwent a moderate fractionation (~20%) of ol + cpx + mg, in proportion that range between 75-40%, 55-10% and 15-0 %, respectively.-
dc.descriptionEste trabajo forma parte del Proyecto de Investigación «El volcanismo del Neógeno-Cuaternario del Borde mediterráneo Ibérico: implicaciones sobre la naturaleza del Manto superior y tectónica asociada», subvencionado por la CAICYT-
dc.descriptionPeer reviewed-
dc.format7162841 bytes-
dc.formatapplication/pdf-
dc.languagespa-
dc.publisherSociedad Geológica de España-
dc.rightsopenAccess-
dc.subjectUpper Mantle-
dc.subjectMediterranean volcanism-
dc.subjectLeucite-basanites-
dc.subjectNepheline-basanites-
dc.subjectOlivine basalts-
dc.subjectPartial melting-
dc.subjectFractional crystallization-
dc.titlePetrogénesis de los basaltos alcalinos de la Garrotxa, región volcánica del NE de España-
dc.typeArtículo-
Appears in Collections:Digital Csic

Files in This Item:
There are no files associated with this item.


Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.