Carbonate melt interaction with natural eclogite at 6 GPa and 1100–1200 °C: Implications for metasomatic melt composition in subcontinental lithospheric mantle › Research Explorer

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Carbonate melt interaction with natural eclogite at 6 GPa and 1100–1200 °C: Implications for metasomatic melt composition in subcontinental lithospheric mantle

Research output: Contribution to journal › Article › peer-review

DOI

https://doi.org/10.1016/j.chemgeo.2020.119915
Final published version

Anton Shatskiy
Altyna Bekhtenova
Ivan V. Podborodnikov
Anton V. Arefiev
Konstantin D. Litasov

Original language	English
Article number	119915
Number of pages	15
Journal	Chemical Geology
Volume	558
DOIs	https://doi.org/10.1016/j.chemgeo.2020.119915
Publication status	Published - 30 Dec 2020

OECD FOS+WOS

1.05.GC GEOCHEMISTRY & GEOPHYSICS
1.05.KY GEOLOGY

Research areas

Carbonatite melt, Continental lithosphere, Eclogite, High-pressure experiment, Mantle metasomatism, Mixed paragenesis, BEARING ECLOGITE, HIGH-PRESSURE, EAST KIMBERLITE, UDACHNAYA KIMBERLITE PIPE, DIAMOND, XENOLITHS, FLUID INCLUSIONS, MINERAL INCLUSIONS, PHASE-RELATIONS, POTASSIUM

ID: 25606084