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Detailed Reference Information |
Liu, L. and Irifune, T. (1998). Comment on “A new hydrous silicate, a water reservoir, in the upper part of the lower mantle” by Eiji Ohtani, Hiroki Mizobata, Yasuhiro Kudoh, Toshiro Nagase, Haruo Arashi, Hisayoshi Yurimoto, and Isoji Miyagi. Geophysical Research Letters 25: doi: 10.1029/98GL00474. issn: 0094-8276. |
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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>. ¿ 1998 American Geophysical Union |
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BACKGROUND DATA FILES |
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Abstract |
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Keywords
Mineralogy and Petrology, Experimental mineralogy and petrology, Mineral Physics, High-pressure behavior |
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Publisher
American Geophysical Union 2000 Florida Avenue N.W. Washington, D.C. 20009-1277 USA 1-202-462-6900 1-202-328-0566 service@agu.org |
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