Wüstite stability in the presence of a CO 2 -fluid and a carbonate-silicate melt: Implications for the graphite/diamond formation and generation of Fe-rich mantle metasomatic agents-Reference-Cited by-同舟云学术

Wüstite stability in the presence of a CO 2 -fluid and a carbonate-silicate melt: Implications for the graphite/diamond formation and generation of Fe-rich mantle metasomatic agents

Published:2016-02 Issue: Volume:244 Page:20-29
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Bataleva Yuliya V.,Palyanov Yuri N.,Sokol Alexander G.,Borzdov Yuri M.,Bayukov Oleg A.

Funder

Russian Science Foundation

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference68 articles.

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4. The role of rocks saturated with metallic iron in the formation of ferric carbonate-silicate melts: experimental modeling under PT-conditions of lithospheric mantle;Bataleva;Russian Geology and Geophysics,2015

5. Thermobarometry using multiequilibrium calculations: a new technique with petrologic applications;Berman;Canadian Mineralogist,1991

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4. Origin of K-rich diamond-forming immiscible melts and CO2 fluid via partial melting of carbonated pelites at a depth of 180–200 km;Gondwana Research;2019-11

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