Oxidation States of Fe in Constituent Minerals of a Spinel Lherzolite Xenolith from the Tariat Depression, Mongolia: The Significance of Fe3+ in Olivine

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言語	英語
著者	Ejima Terumi Faculty of Science, Shinshu University, 3-1-1, Asahi, Matsumoto 390-8621, Japan Osanai Yasuhito Division of Evolution of Earth Environments, Graduate School of Social, Cultural Studies, Kyushu University, Fukuoka 810-8560, Japan Akasaka Masahide Department of Geoscience, Graduate School of Science and Engineering, Shimane University, Matsue 690-8504, Japan Adachi Tatsuro Division of Evolution of Earth Environments, Graduate School of Social, Cultural Studies, Kyushu University, Fukuoka 810-8560, Japan Nakano Nobuhiko Division of Evolution of Earth Environments, Graduate School of Social, Cultural Studies, Kyushu University, Fukuoka 810-8560, Japan Kon Yoshiaki Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), Tsukuba 305-8567, Japan Ohfuji Hiroaki Geodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan Sereenen Jargalan School of Geology and Mining Engineering, Mongolian University of Science and Technology, Ulaanbaatar 14191, Mongolia
主題	spinel lherzolite xenolith; oxidation state of Fe; Fe-57 Mossbauer spectroscopy; Mongolia; Tariat Depression
掲載誌名	MINERALS
巻	8
号	5
ISSN（Online）	2075-163X
発行日	2018-05
DOI	10.3390/min8050204
出版者	MDPI
資料タイプ	学術雑誌論文
部局	総合理工学部
備考	We thank Fujio Izumi and Koichi Momma of the National Institute for Materials Science for their permission to use the RIETAN-FP and VESTA programs. We appreciate valuable and constructive comments by three anonymous reviewers. This work was supported by a Grant-in-Aid for Research Activity Start-up from the Japan Society for the Promotion of Science (JSPS).