Comment on ``A new hydrous silicate, a water reservoir, in the upper part of the lower mantle''

Details Comment on ``A new hydrous silicate, a water reservoir, in the upper part of the lower mantle'' Comment on ``A new hydrous silicate, a water reservoir, in the upper part of the lower mantle''

Apr 1998

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1998georl..25..979l&link_type=abstract

Geophysical Research Letters, Volume 25, Issue 7, p. 979-980

Physics

2

Mineralogy And Petrology: Experimental Mineralogy And Petrology, Mineral Physics: High-Pressure Behavior

Scientific paper

On the basis of the available powder X-ray diffraction data, chemical composition, Raman spectrum and synthesis P-T conditions, it is concluded that the so-called new phase claimed by Ohtani et al. [1997] is in reality the phase D reported earlier by Liu [1987], Irifune et al. [1996] and Kuroda and Irifune [1997]. Phase F first reported by Kanzaki [1991] is also probably in reality the phase D. The powder X-ray diffraction pattern of the so-called phase F studied by Kudoh et al. [1995] bears no resemblance to that reported by Kanzaki [1991], suggesting a totally different material was employed in the study of Kudoh et al. [1995].

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