Peritectic Reaction of Olivine in the Olivine–Jadeite–Diopside–Garnet–(C–O–H) System at 6 GPa as the Key Mechanism of the Magmatic Evolution in the Upper Mantle

Author:

Litvin Yu. A.,Kuzyura A. V.

Publisher

Pleiades Publishing Ltd

Subject

Geochemistry and Petrology,Geophysics

Reference64 articles.

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3. R. L. Bates and J. A. Jackson, Dictionary of Geological Terms, Third edition (Ancor Books, Doubleday, New York, 1983).

4. P. M. Bell and B. T. C. Davis, “Melting relations in the system jadeite– diopside at 30 and 40 kb,” Am. J. Sci. A–267, 17–32 (1969).

5. A. P. Bobrievich, M. N. Bondarenko, L. M. Gnevushev, L. M. Krasov, G. I, Smirnov, and R. K. Yurkevich, Diamond Deposits of Yakutia (Geogeoltekhizdat, Moscow, 1959) [in Russian].

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