DOI: 10.1029/98gl00542. Reply [to “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”]

Reply [to “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”]

10.1029/98gl00542

Crossref journal-article

American Geophysical Union (AGU)

Geophysical Research Letters (13)

Abstract

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 realy 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].

Bibliography

Ohtani, E., Mizobata, H., Kudoh, Y., Nagase, T., Arashi, H., Yurimoto, H., & Miyagi, I. (1998). Reply [to âComment on âA new hydrous silicate, a water reservoir, in the upper part of the lower mantleâ by Eiji Ohtani, Hiroki Mizobata, Yasuhiro Kudoh, Toshiro Nagase, Haruo Arashi, Hisayoshi Yurimoto, and Isoji Miyagiâ]. Geophysical Research Letters, 25(7), 981â982. Portico.

Authors 7

Eiji Ohtani (first)
Hiroki Mizobata (additional)
Yasuhiro Kudoh (additional)
Toshiro Nagase (additional)
Haruo Arashi (additional)
Hisayoshi Yurimoto (additional)
Isoji Miyagi (additional)

References 12 Referenced 3

{'key': 'e_1_2_2_2_1', 'first-page': '41', 'volume-title': 'Powder diffraction file, Inorganic and organic', 'author': 'JCPDS', 'year': '1991'} / Powder diffraction file, Inorganic and organic by JCPDS (1991)
10.1016/0031-9201(91)90085-V
10.1007/BF00202769
10.1029/97GL00875
Kudoh Y.T.NagaseH.MizobataE.OhtaniS.SasakiM.Tanaka Possible sites for hydrogen in a new hydrous magnesium silicate phase G synthesized at 22 GPa and 1050°C Proceedings for AIRAPT16 Kyoto August 24–29 1997b (10.1029/97GL00875)
10.1007/s002690050078
10.1029/GM101p0545
10.1038/350332a0
10.1016/0031-9201(87)90138-5
10.1029/97GL00874
10.2465/minerj.20.163
10.2138/am-1997-5-627

Dates

Type	When
Created	21 years, 6 months ago (Feb. 3, 2004, 11:36 p.m.)
Deposited	1 year, 9 months ago (Nov. 22, 2023, 5:32 a.m.)
Indexed	1 year, 9 months ago (Nov. 22, 2023, 6:10 a.m.)
Issued	27 years, 4 months ago (April 1, 1998)
Published	27 years, 4 months ago (April 1, 1998)
Published Online	27 years, 4 months ago (April 1, 1998)
Published Print	27 years, 4 months ago (April 1, 1998)

Funders 0

None

BibTeX

@article{Ohtani_1998, title={Reply [to “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”]}, volume={25}, ISSN={1944-8007}, url={http://dx.doi.org/10.1029/98gl00542}, DOI={10.1029/98gl00542}, number={7}, journal={Geophysical Research Letters}, publisher={American Geophysical Union (AGU)}, author={Ohtani, Eiji and Mizobata, Hiroki and Kudoh, Yasuhiro and Nagase, Toshiro and Arashi, Haruo and Yurimoto, Hisayoshi and Miyagi, Isoji}, year={1998}, month=apr, pages={981–982} }

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