Preferential dissolution of SiO2 from enstatite to H2 fluid under high pressure and temperature-Reference-Cited by-同舟云学术

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Preferential dissolution of SiO2 from enstatite to H2 fluid under high pressure and temperature

Published:2015-12-24 Issue:4 Volume:43 Page:277-285
ISSN:0342-1791
Container-title:Physics and Chemistry of Minerals
language:en
Short-container-title:Phys Chem Minerals

Author:

Shinozaki Ayako,Kagi Hiroyuki,Hirai Hisako,Ohfuji Hiroaki,Okada Taku,Nakano Satoshi,Yagi Takehiko

Funder

Japan Society for the Promotion of Science

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,General Materials Science

Link

http://link.springer.com/content/pdf/10.1007/s00269-015-0792-3.pdf

Reference29 articles.

1. Abebe M, Walrafen GE (1979) Raman studies of ice-VI using a diamond anvil cell. J Chem Phys 71:4167–4169. doi: 10.1063/1.438190

2. Bali E, Audétat A, Keppler H (2013) Water and hydrogen are immiscible in Earth’s mantle. Nature 495:220–222

3. Ballhaus C (1995) Is the upper mantle metal-saturated? Earth Planet Sci Lett 132:75–86

4. Boyd F, England J, Davis BT (1964) Effects of pressure on the melting and polymorphism of enstatite, MgSiO3. J Geophys Res 69:2101–2109

5. Chen CH, Presnall DC (1975) System Mg2SiO4–SiO2 at pressures up to 25 kilobars. Am Miner 60:398–406

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2. Chemical reaction of the reduced carbon and hydrogen species and effect on phase relation of the silicate minerals under the interior of the Earth;Japanese Magazine of Mineralogical and Petrological Sciences;2020

3. Three-dimensional X-ray topographic characterization of broken and unbroken natural diamond anvil crystals at 99.4 GPa;Transactions of the Materials Research Society of Japan;2019-08-01

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