Solidus of carbonated peridotite and basalt to 33 GPa with implication to origin of kimberlite- and carbonatite-like melts in the deep mantle

K.D. Litasov; S. Ghosh; E. Ohtani

doi:10.29173/ikc3387

Solidus of carbonated peridotite and basalt to 33 GPa with implication to origin of kimberlite- and carbonatite-like melts in the deep mantle

Authors

K.D. Litasov
S. Ghosh
E. Ohtani

DOI:

https://doi.org/10.29173/ikc3387

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Published

2008-10-15

How to Cite

Litasov, K., Ghosh, S., & Ohtani, E. (2008). Solidus of carbonated peridotite and basalt to 33 GPa with implication to origin of kimberlite- and carbonatite-like melts in the deep mantle. International Kimberlite Conference: Extended Abstracts, 9. https://doi.org/10.29173/ikc3387

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Issue

Vol. 9 (2008): Vol 9: International Kimberlite Conference, Frankfurt

Section

Extended Abstracts

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