Solidus of carbonated phlogopite eclogite at 3–6 GPa: Implications for mantle metasomatism and ultra-high pressure metamorphism
Author:
Funder
Russian Science Foundation
Publisher
Elsevier BV
Subject
Geology
Reference123 articles.
1. Geochemistry of eclogite xenoliths from the Udachnaya Kimberlite Pipe: Section of ancient oceanic crust sampled;Agashev;Lithos,2018
2. Nature of diamonds in Yakutian eclogites: views from eclogite tomography and mineral inclusions in diamonds;Anand;Lithos,2004
3. The system K2CO3–CaCO3–MgCO3 at 3 GPa: Implications for carbonatite melt compositions in the subcontinental lithospheric mantle;Arefiev;Minerals,2019
4. The K2CO3–CaCO3–MgCO3 system at 6 GPa: implications for diamond forming carbonatitic melts;Arefiev;Minerals,2019
5. Aulbach, S., Höfer, H.E., Gerdes, A., 2019. High-Mg and low-Mg mantle eclogites from Koidu (West African Craton) linked by Neoproterozoic ultramafic melt metasomatism of subducted Archaean plateau-like oceanic crust. J. Petrology 60, 723-754.
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1. The NaCl–CaCO3–MgCO3 System at 3 GPa: Implications for Mantle Solidi;Russian Geology and Geophysics;2023-08-01
2. The System KCl–CaCO3–MgCO3 at 3 GPa;Minerals;2023-02-09
3. Change in carbonate budget and composition during subduction below metal saturation boundary;Geoscience Frontiers;2023-01
4. Ti and Cr in High-Pressure Mica: Experimental Study and Application to the Mantle Assemblages;Petrology;2022-12
5. Metasomatized Xenoliths of Mantle Eclogites and Garnet Pyroxenites from the V. Grib Kimberlite, Arkhangelsk Province;Petrology;2022-09-06
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