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

Citation

Kamenetsky, V, Sobolev, A, Eggins, S et al. 2002, '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, vol. 183, pp. 287-303.

Year

2002

Field of Research

  • Igneous And Metamorphic Petrology

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