Phase relations in the peridotite–carbonate–chloride system at 7.0–16.5 GPa and the role of chlorides in the origin of kimberlite and diamond

Chemical Geology - Tập 262 Số 1-2 - Trang 29-41 - 2009
Konstantin D. Litasov1, Eiji Ohtani2
1Geophysical Laboratory, Carnegie Institution of Washington, Washington DC 20015 USA
2Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University, Sendai 980-8578, Japan

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