Effects of Grain Size, Cooling Rate, and Sample Preparation on the Phase Transition from Protoenstatite to Clinoenstatite
Author:
Affiliation:
1. Faculty of Education, Shiga University, 2-5-1 Hiratsu, Otsu, 520-0862, Japan
2. Graduate School of Science, Kyoto University, Kitashirakawa-Oiwake, Sakyo, Kyoto, 606-8502, Japan
Abstract
Publisher
Mineralogical Association of Canada
Subject
Geochemistry and Petrology
Link
https://pubs.geoscienceworld.org/canmin/article-pdf/60/3/405/5617019/i1499-1276-60-3-405.pdf
Reference22 articles.
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2. Bowe, R.C., Muldawer, L., & Chambers,F. (1970) The effect of particle size on the martensitic transformation of β'-AuZn(50% Zn). Scripta Metallurgica4, 581– 582.
3. Boysen, H., Frey, F., Schrader, H., & Eekold,G. (1991) On the proto- to ortho-/clino enstatite phase transformation: Single crystal X-ray and inelastic neutron investigation. Physics and Chemistry of Minerals17, 629– 635.
4. Chen, I.W., Chiao, Y.H., & Tsuzaki,K. (1985) Statics of martensitic nucleation. Acta Metallurgica33, 1847– 1859.
5. Foster, W.R. (1951) High-temperature X-ray diffraction study of the polymorphism of MgSiO3. Journal of the American Ceramic Society34, 255– 259.
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