Thermal equation of state of MgSiO4H2 phase H determined by in situ X-ray diffraction and a multianvil apparatus
Author:
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/article/10.1007/s00269-018-0980-z/fulltext.html
Reference40 articles.
1. Bindi L, Nishi M, Tsuchiya J, Irifune T (2014) Crystal chemistry of dense hydrous magnesium silicates: the structure of phase H, MgSiH2O4, synthesized at 45 GPa and 1000 °C. Am Miner 99:1802–1805
2. Frost DJ, Fei Y (1998) Stability of phase D at high pressure and high temperature. J Geophys Res 103:7463–7474
3. Gleason AE, Jeanloz R, Kunz M (2008) Pressure–temperature stability studies of FeOOH using X-ray diffraction. Am Miner 93:1882–1885
4. Gleason AE, Quiroga CE, Suzuki A, Pentcheva R, Mao WL (2013) Symmetrization driven spin transition in ε-FeOOH at high pressure. Earth Planet Sci Lett 379:49–55
5. Holl CM, Smyth JR, Manghnani MH, Amulele GM, Sekar M, Frost DJ, Prakapenka VB, Shen G (2006) Crystal structure and compression of an iron-bearing Phase A to 33 GPa. Phys Chem Miner 33:192–199
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