The composition of garnet as an indicator of the conditions of peridotite-carbonatite interaction in the subcratonic lithosphere (experimental data)

Sokol A. G.; Kruk A. N.; Chebotarev D. A.; Palyanov Yu. N.; Sobolev N. V.

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The composition of garnet as an indicator of the conditions of peridotite-carbonatite interaction in the subcratonic lithosphere (experimental data)

机译：石榴石的成分可指示下克拉通岩石圈中橄榄岩-碳酸盐岩相互作用的条件（实验数据）

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《Doklady Earth Sciences》 |2015年第1期|746-750|共5页
作者
Sokol A. G.; Kruk A. N.; Chebotarev D. A.; Palyanov Yu. N.; Sobolev N. V.;
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Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk 630090, Russia;

Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk 630090, Russia;

Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk 630090, Russia;

Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk 630090, Russia;

Russian Acad Sci, Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk, Russia|Novosibirsk State Univ, Novosibirsk 630090, Russia;

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The composition of garnet as an indicator of the conditions of peridotite-carbonatite interaction in the subcratonic lithosphere (experimental data)

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