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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

✍ Scribed by V.S Kamenetsky; A.V Sobolev; S.M Eggins; A.J Crawford; R.J Arculus


Book ID
117072830
Publisher
Elsevier Science
Year
2002
Tongue
English
Weight
653 KB
Volume
183
Category
Article
ISSN
0009-2541

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