In situ X–ray diffraction study of the phase boundary between diaspore and δ–AlOOH
Author:
Affiliation:
1. Department of Earth Science, Graduate School of Science, Tohoku University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/117/1/117_211215/_pdf
Reference21 articles.
1. Abe, R., Shibazaki, Y., Ozawa, S., Ohira, I., et al (2018) In situ X–ray diffraction studies of hydrous aluminosilicate at high pressure and high temperature. Journal of Mineralogical and Petrological Sciences, 113, 106–111.
2. Brown, J.M. (1999) The NaCl pressure standard. Journal of Applied Physics, 86, 5801–5808.
3. Cedillo, A., Torrent, M. and Cortona, P. (2016) Stability of the different AlOOH phases under pressure. Journal of Physics: Condensed Matter, 28, 185401.
4. Chenavas, J., Joubert, J.C., Capponi, J.J. and Marezio, M. (1973) Synthese de nouvelles phases denses d’oxyhydrosydes M3+OOH des metaux de la premiere serie de transition, en milieu hydrothermal à tres haute pression. Journal of Solid State Chemistry, 6, 1–15.
5. Deer, W.A., Howie, R.A. and Zussman, J. (2013) An Introduction to the Rock–Forming Minerals (3rd edition). pp. 498, The Mineralogical Society, London.
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1. Electron density changes accompanying high-pressure phase transition in AlOOH;Mineralogical Magazine;2024-04-11
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