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