Please use this identifier to cite or link to this item: http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2892
Full metadata record
DC FieldValueLanguage
dc.creatorAparicio, Alfredo-
dc.creatorBustillo, Mª Ángeles-
dc.creatorGarcía García, Roberto-
dc.creatorAraña, Vicente-
dc.date2008-02-08T08:11:11Z-
dc.date2008-02-08T08:11:11Z-
dc.date2006-
dc.date.accessioned2017-01-31T00:59:47Z-
dc.date.available2017-01-31T00:59:47Z-
dc.identifierGeological Magazine vol 143 paginas 181-193-
dc.identifierhttp://hdl.handle.net/10261/2892-
dc.identifier10.1017/S0016756806001713-
dc.identifier.urihttp://dspace.mediu.edu.my:8181/xmlui/handle/10261/2892-
dc.descriptionThe xenoliths of dunites and other ultramafic rocks (peridotites ,wherlites..etc) are generated by contact metamorphism from sedimentary rocks-
dc.descriptionproyecto FEDER "Aspectos educativos del volcanismo canario Ministerio Educación Y Ciencia proyecto BTE2002-04017-Co2-1-
dc.descriptionPeer reviewed-
dc.format1106 bytes-
dc.formattext/html-
dc.languageeng-
dc.publisherCambridge University Press-
dc.rightsopenAccess-
dc.subjectmetasedimentary xenoliths-
dc.subjectdunites-
dc.titleMetasedimentary xenoliths in the lavas of the Timanfaya eruption(1730-1736. Lanzarote, Canary Islands):metamorphism and contamination processes-
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.