Apr 1998
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998georl..25..981o&link_type=abstract
Geophysical Research Letters, Volume 25, Issue 7, p. 981-982
Physics
1
Mineral Physics: Optical, Infrared, And Raman Spectroscopy, Mineralogy And Petrology: Experimental Mineralogy And Petrology, Mineral Physics: High-Pressure Behavior
Scientific paper
Phase G reported by Ohtani et al. [1997] and Kudoh et al. [1997a] is identical with the new phase D reported by Kuroda and Irifune [1998] and Yang et al. [1997]. However, there is ambiguity on existence of phase D defined by Liu [1987]. There are following possibilities on existence of Liu's phase D; (1) the product was a mixture of phase G and the other contaminant phases, (2) it really exists stably in different pressure and temperature conditions from those studied by our works, or (3) the phase is a metastable phase formed due to a short run duration and/or no sealing of water in the diamond anvil cell. Therefore, it is not appropriate to use the name phase D for the dense hydrous magnesium silicate phase G reported by us [Ohtani et al., 1997].
Arashi Haruo
Kudoh Yasuhiro
Miyagi Isoji
Mizobata Hiroki
Nagase Toshiro
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