Akasaka, M.

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Journal Article

Nagashima, M.; Armbruster, T.; Akasaka, M.; Minakawa, T. (2010). Crystal chemistry of Mn2+-, Sr-rich REE-bearing piemontite from Kamisigai mine in the Sambagawa metamorphic belt, Shikoku, Japan. Journal of mineralogical and petrological sciences, 105(3), pp. 142-150. Sendai (Jap.): Mineralogical Society of Japan, and the Japanese Association of Mineralogists, Petrologists and Economic Geologists 10.2465/jmps.090709

Nagashima, Mariko; Akasaka, M.; Minakawa, T.; Libowitzky, E.; Armbruster, Thomas Michael (2009). Sursassite: Hydrogen bonding, cation order, and pumpellyite intergrowth. American mineralogist, 94(10), pp. 1440-1449. Mineralogical Society of America 10.2138/am.2009.3223

Nagashima, N.; Rahmoun, N.S.; Alekseev, E.; Geiger, C.A.; Armbruster, T.; Akasaka, M. (2008). Crystal chemistry of macfallite: Relationships to sursassite and pumpellyite. American mineralogist, 93(11-12), pp. 1851-1857. Washington, D.C.: Mineralogical Society of America 10.2138/am.2008.2935

Nagashima, Mariko; Akasaka, M. (2007). THE DISTRIBUTION OF CHROMIUM IN CHROMIAN PUMPELLYITE FROM SARANI, URALS, RUSSIA: A TOF NEUTRON AND X-RAY RIETVELD STUDY. The Canadian Mineralogist, 45(4), pp. 837-846. Mineralogical Association of Canada 10.2113/gscanmin.45.4.837

Nagashima, Mariko; Akasaka, M.; Sakurai, T. (2006). Chromian epidote in omphacite rocks from the Sambagawa metamorphic belt, central Shikoku, Japan. Journal of mineralogical and petrological sciences, 101, pp. 157-169. Mineralogical Society of Japan, and the Japanese Association of Mineralogists, Petrologists and Economic Geologists

Akasaka, M.; Nagashima, Mariko; Makino, K.; Ohashi, H. (2005). Distribution of Fe3+ in a synthetic (Ca,Na)2(Mg,Fe3+)Si2O7-melilite: 57Fe Mössbauer and X-ray Rietveld studies. Journal of mineralogical and petrological sciences, 100, pp. 229-236. Mineralogical Society of Japan, and the Japanese Association of Mineralogists, Petrologists and Economic Geologists

Nagashima, Mariko; Akasaka, M. (2004). An X-ray Rietveld study of piemontite on the join Ca2Al3Si3O12(OH) - Ca2Mn3+3Si3O12(OH) formed by hydrothermal synthesis. American mineralogist, 89(7), pp. 1119-1129. Mineralogical Society of America

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