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
V.S Kamenetsky, A.V Sobolev, S.M Eggins, A.J Crawford, R.J ArculusVolume:
183
Year:
2002
Language:
english
DOI:
10.1016/s0009-2541(01)00380-1
File:
PDF, 653 KB
english, 2002