Akimotoite, a new mineral discovered in a shocked meteorite
Author:
Affiliation:
1. Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology
Publisher
Japan Association of Mineralogical Sciences
Subject
Economic Geology,Geochemistry and Petrology
Link
https://www.jstage.jst.go.jp/article/gkk/53/1/53_231002/_pdf
Reference12 articles.
1. Gasparik, T. (1990): Phase relations in the transition zone. J. Geophys. Res.: Solid Earth, 95, 15751-15769.
2. Madon, M. and Poirier, J.P. (1983): Transmission electron microscope observation of α, β and γ (Mg,Fe)2SiO4 in shocked meteorites: planar defects and polymorphic transitions. Phys. Earth Planet. Inter., 33, 31-44.
3. Miyahara, M., Tomioka, N. and Bindi, L. (2021): Natural and experimental high-pressure, shock-produced terrestrial and extraterrestrial materials. Prog. Earth Planet. Sci., 8, 59.
4. Miyahara, M., Yamaguchi, A., Saitoh, M., Fukimoto, K., Sakai, T., Ohfuji, H., Tomioka, N., Kodama, Y. and Ohtani, E. (2020): Systematic investigations of high-pressure polymorphs in shocked ordinary chondrites. Meteorit. Planet. Sci., 55, 2619-2651.
5. Sharp, T.G., Lingemann, C.M., Dupas, C. and Stoffler, D. (1997): Natural occurrence of MgSiO3-ilmenite and evidence for MgSiO3-perovskite in a shocked L chondrite. Science, 277, 352-355.
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