Variable–temperature single–crystal X–ray diffraction study of SrGeO3 high–pressure perovskite phase
Author:
Affiliation:
1. Graduate School of Sciences and Technology for Innovation, Yamaguchi University
2. Graduate School of Science and Technology, Kumamoto University
3. Graduate School of Science, Osaka University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/113/6/113_180605/_pdf
Reference18 articles.
1. Akaogi, M., Kojitani, H., Yusa, H., Yamamoto, R., Kido, M. and Koyama, K. (2005) High–pressure transitions and thermochemistry of MGeO3 (M = Mg, Zn and Sr) and Sr–silicates: systematics in enthalpies of formation of A2+B4+O3 perovskites. Physics and Chemistry of Minerals, 32, 603–613.
2. Andrault, D., Itié, J.–P. and Farges, F. (1996) High–temperature structural study of germanate perovskites and pyroxenoids. American Mineralogist, 81, 822–832.
3. Becker, P.J. and Coppens, P. (1974a) Extinction within the limit of validity of the Darwin transfer equations. I. General formalisms for primary and secondary extinction and their application to spherical crystals. Acta Crystallographica, A30, 129–147.
4. Becker, P.J. and Coppens, P. (1974b) Extinction within the limit of validity of the Darwin transfer equations. II. Refinement of extinction in spherical crystals of SrF2 and LiF. Acta Crystallographica, A30, 148–153.
5. Durben, D.J., Wolf, G.H. and McMillan, P.F. (1991) Raman scattering study of the high–temperature vibrational properties and stability of CaGeO3 perovskite. Physics and Chemistry of Minerals, 18, 215–223.
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