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Metasedimentary xenoliths in the lavas of the Timanfaya eruption(1730-1736. Lanzarote, Canary Islands):metamorphism and contamination processes

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dc.creator Aparicio, Alfredo
dc.creator Bustillo, Mª Ángeles
dc.creator García García, Roberto
dc.creator Araña, Vicente
dc.date 2008-02-08T08:11:11Z
dc.date 2008-02-08T08:11:11Z
dc.date 2006
dc.date.accessioned 2017-01-31T00:59:47Z
dc.date.available 2017-01-31T00:59:47Z
dc.identifier Geological Magazine vol 143 paginas 181-193
dc.identifier http://hdl.handle.net/10261/2892
dc.identifier 10.1017/S0016756806001713
dc.identifier.uri http://dspace.mediu.edu.my:8181/xmlui/handle/10261/2892
dc.description The xenoliths of dunites and other ultramafic rocks (peridotites ,wherlites..etc) are generated by contact metamorphism from sedimentary rocks
dc.description proyecto FEDER "Aspectos educativos del volcanismo canario Ministerio Educación Y Ciencia proyecto BTE2002-04017-Co2-1
dc.description Peer reviewed
dc.format 1106 bytes
dc.format text/html
dc.language eng
dc.publisher Cambridge University Press
dc.rights openAccess
dc.subject metasedimentary xenoliths
dc.subject dunites
dc.title Metasedimentary xenoliths in the lavas of the Timanfaya eruption(1730-1736. Lanzarote, Canary Islands):metamorphism and contamination processes
dc.type Artículo


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