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The xenoliths of dunites and other ultramafic rocks (peridotites ,wherlites..etc) are generated by contact metamorphism from sedimentary rocksproyecto FEDER "Aspectos educativos del volcanismo canario\udMinisterio Educación Y Ciencia proyecto BTE2002-04017-Co2-1Peer reviewe

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