Experimental Study of the Peridotite-H2O System at P=3.8-4 GPa and T=1000-1400 degrees C: Critical Relations and Vertical Zoning of the Upper Mantle

Gorbachev N. S.; Kostyuk A. V.; Shapovalov Yu. B.

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Experimental Study of the Peridotite-H2O System at P=3.8-4 GPa and T=1000-1400 degrees C: Critical Relations and Vertical Zoning of the Upper Mantle

机译：橄榄岩-H2O系统在P = 3.8-4 GPa和T = 1000-1400摄氏度的实验研究：上地幔的临界关系和垂直分区

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《Doklady Earth Sciences》 |2015年第2期|360-363|共4页
作者
Gorbachev N. S.; Kostyuk A. V.; Shapovalov Yu. B.;
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Russian Acad Sci, Inst Expt Mineral, Chernogolovka 142432, Moscow Oblast, Russia;

Russian Acad Sci, Inst Expt Mineral, Chernogolovka 142432, Moscow Oblast, Russia;

Russian Acad Sci, Inst Expt Mineral, Chernogolovka 142432, Moscow Oblast, Russia;

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Experimental Study of the Peridotite-H2O System at P=3.8-4 GPa and T=1000-1400 degrees C: Critical Relations and Vertical Zoning of the Upper Mantle

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