 | GOTO, Atsushi, KUNUGIZA, Keitaro, MIYAJIMA, Hiroshi (2017) Phase relation in the NaAlSiO4–SiO2–H2O system for the hydrothermal precipitation of jadeite, albite, natrolite, and analcime in jadeitite of the Itoigawa–Omi area, Japan. Journal of Mineralogical and Petrological Sciences, 112 (5) 271-280 doi:10.2465/jmps.170402b | Journal (article/letter/editorial) | | natrolite, and analcime in jadeitite of the Itoigawa–Omi area, Japan Atsushi GOTO*, Keitaro KUNUGIZA** and...Institute of Technology), Himeji, Hyogo 671–2280, Japan ** Department of Environment and Humanity, Faculty...930–8555, Japan *** Fossa Magna Museum, 1313 Ichinomiya Itoigawa, Niigata 941–0056, Japan Jadeitite...Jadeitite from the Itoigawa–Omi area in the Hida–Gaien belt is hydrothermal in origin, occurring as tectonic blocks..., 2012), Myanmar (e.g., Shi et al., 2012), and Japan (Miyajima et al., 1999). Jadeitite occurs generally |  | | Journal (article/letter/editorial) | | Ore Deposit in the Hida Metamorphic Belt, Central Japan : Leaching and Precipitation of Clinopyroxene Keitaro...skarn deposit in the Hida metamorphic belt, central Japan (cf. Kano et al., 1992), clinopyroxene occurs both...Education, Toyama University, Toyama 930-8555, Japan [e-mail: kunugiza@edu.toyama-u.ac.jp] Keywords:...skarn 199 200 K. KUNUGIZA RESOURCE GEOLOGY : Japan Sea Hida gneiss and limestone Hida meta-granite...ore deposit in the Hida metamorphic belt, central Japan. Akiyama, 1980), Shimazaki and Kusakabe (1990) |  | | Journal (issue) | | I loved this time of day, as the perpetual noisy city dropped to absolute silence. Not a vehicle was on...will close its doors this year as a result of the City of Tucson taking over the property for residential...for Gilgit. We made a few stops in this largest city of the Northern Areas, both prearranged and by luck...pyrope 1.04% FeiOi andradite 4.67% CaO grossular 0.96% TOTAL 100.00% Energy Dispersive Spectroscopy...from the bed of the Kotakioawa River at Itoigawa City, central Japan. Associated mineral; are jadeite, natrolite |
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