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Xu, Chaowen, Inoue, Toru (2019) Phase Relations in MAFSH System up to 21 GPa: Implications for Water Cycles in Martian Interior. Minerals, 9 (9) 559 doi:10.3390/min9090559

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Reference TypeJournal (article/letter/editorial)
TitlePhase Relations in MAFSH System up to 21 GPa: Implications for Water Cycles in Martian Interior
JournalMinerals
AuthorsXu, ChaowenAuthor
Inoue, ToruAuthor
Year2019 (September 16)Volume9
Issue9
PublisherMDPI AG
URL
Download URLhttps://www.mdpi.com/2075-163X/9/9/559/pdf?version=1568721765
DOIdoi:10.3390/min9090559Search in ResearchGate
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Mindat Ref. ID7736241Long-form Identifiermindat:1:5:7736241:0
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Full ReferenceXu, Chaowen, Inoue, Toru (2019) Phase Relations in MAFSH System up to 21 GPa: Implications for Water Cycles in Martian Interior. Minerals, 9 (9) 559 doi:10.3390/min9090559
Plain TextXu, Chaowen, Inoue, Toru (2019) Phase Relations in MAFSH System up to 21 GPa: Implications for Water Cycles in Martian Interior. Minerals, 9 (9) 559 doi:10.3390/min9090559
In(2019, September) Minerals Vol. 9 (9) MDPI AG

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Xu, Chaowen, Gréaux, Steeve, Inoue, Toru, Noda, Masamichi, Gao, Jing, Li, Ying (2022) Sound Velocities of Superhydrous Phase B up to 21 GPa and 900 K. Geophysical Research Letters, 49 (13) doi:10.1029/2022gl098674
Xu, Chaowen, Inoue, Toru (2019) Melting of Al‐Rich Phase D up to the Uppermost Lower Mantle and Transportation of H 2 O to the Deep Earth. Geochemistry, Geophysics, Geosystems, 20 (9) 4382-4389 doi:10.1029/2019gc008476
Ohnishi, Satoka, Kuwayama, Yasuhiro, Inoue, Toru (2017) Melting relations in the MgO–MgSiO3 system up to 70 GPa. Physics and Chemistry of Minerals, 44 (6) 445-453 doi:10.1007/s00269-017-0871-8
Inoue, Toru (1994) Effect of water on melting phase relations and melt composition in the system Mg2SiO4MgSiO3H2O up to 15 GPa. Physics of the Earth and Planetary Interiors, 85 (3). 237-263 doi:10.1016/0031-9201(94)90116-3
Xu, Chaowen, Gréaux, Steeve, Inoue, Toru, Noda, Masamichi, Sun, Wei, Kuwahara, Hideharu, Higo, Yuji (2020) Sound Velocities of Al‐Bearing Phase D up to 22 GPa and 1300 K. Geophysical Research Letters, 47 (18) doi:10.1029/2020gl088877
Xu, Chaowen, Inoue, Toru, Kakizawa, Sho, Noda, Masamichi, Gao, Jing (2021) Effect of Al on the stability of dense hydrous magnesium silicate phases to the uppermost lower mantle: implications for water transportation into the deep mantle. Physics and Chemistry of Minerals, 48 (9) doi:10.1007/s00269-021-01156-4
Xu, Chaowen, Inoue, Toru, Gao, Jing, Noda, Masamichi, Kakizawa, Sho (2022) Melting phase relation of Fe-bearing Phase D up to the uppermost lower mantle. American Mineralogist, 107 (3) 343-349 doi:10.2138/am-2021-7907
Arefiev, Anton V., Shatskiy, Anton, Podborodnikov, Ivan V., Litasov, Konstantin D. (2019) The K2CO3–CaCO3–MgCO3 System at 6 GPa: Implications for Diamond Forming Carbonatitic Melts. Minerals, 9 (9) 558 doi:10.3390/min9090558
Fabrichnaya, O.B. (1999) The phase relations in the FeO-MgO-Al2O3-SiO2 system: assessment of thermodynamic properties and phase equilibria at pressures up to 30 GPa. Calphad, 23 (1) 19-67 doi:10.1016/s0364-5916(99)00013-9
A., , B.T., , V., , M., (2019) High‐Temperature Evolution of Point Defect Equilibria in Hydrous Forsterite Synthesized at 1100 °C and up to 4 GPa. Minerals, 9 (10) 574 doi:10.3390/min9100574
Hermann, Jörg, Troitzsch, Ulrike, Scott, Dean (2016) Experimental subsolidus phase relations in the system CaCO3–CaMg(CO3)2 up to 6.5 GPa and implications for subducted marbles. Contributions to Mineralogy and Petrology, 171 (10) doi:10.1007/s00410-016-1296-y
 
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