Olivine-enriched melt inclusions in chromites from low-Ca boninites, Cape Vogel, Papua New Guinea: Evidence for ultramafic primary magma, refractory mantle source and enriched components

Chemical Geology

Volumn 183, Issue 1-4, 2002, Pages 287-303

  Kamenetsky, V S ^a   Sobolev, A V ^b,c   Eggins, S M ^d   Crawford, A J ^a   Arculus, R J ^d  

^a UNIVERSITY OF TASMANIA   (Australia)

^b VERNADSKY INSTITUTE OF GEOCHEMISTRY AND ANALYTICAL CHEMISTRY   (Russian Federation)

^c MAX PLANCK INSTITUTE FOR CHEMISTRY   (Germany)

^d AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

Author keywords

Mantle; Melt; Spinel

Indexed keywords

BONINITE; CHROMITE; CONFERENCE PROCEEDING; ENRICHMENT; MAGMA CHEMISTRY; MANTLE SOURCE; MELT INCLUSION;

PAPUA NEW GUINEA;

EID: 0036204468     PISSN: 00092541     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0009-2541(01)00380-1     Document Type: Article

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