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岩手大学 教育学部

地学教室
岩石学研究室

Petrological Laboratory

Petrological
Laboratory

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研究・発表

英語原著論文(査読あり)

  • Naemura, K., Erdenejargal, C., Javkhlan, T.O., Kato, T. and Hirajima, T., Geochronology and tectonic implications of the Urgamal eclogite, Western Mongolia. Journal of Mineralogical and Petrological Sciences, 115, pp.357-364, DOI:10.2465/jmps.191126, 2020.
  • Naemura, K., Hirajima, T., Svojtka, M., Shimizu, I. and Iizuka, T., Fossilized melts in mantle wedge peridotites. Scientific Reports, DOI:10.1038/s41598-018-28264-6, 2018.
  • Naemura, K., Shimizu, I., Svojtka, M. and Hirajima, T., Accessory priderite and burbankite in multiphase solid inclusions in the orogenic garnet peridotite from the Bohemian Massif, Czech Republic, Journal of Mineralogical and Petrological Sciences, 110, pp. 20-28, 2015.
  • Obata, M., Ozawa, K., Naemura, K. and Miyake, A., Isochemical breakdown of garnet in orogenic garnet peridotite and its implication to reaction kinetics , Mineralogy and Petrology, 107, pp. 881-895, 2013.
  • Naemura, K., Ikuta, D., Kagi, H., Odake, S., Ueda, T., Ohi, S., Kobayashi, T., Svojtka, M. and Hirajima, T. Diamond and other possible ultra-deep evidence discovered in the orogenic spinel-garnet peridotite from the Moldanubian zone of the Bohemian Massif, Czech Republic. In: Ultrahigh-Pressure metamorphism, edited by Dobrzhinetskaya, R., Faryad, S.W., Wallis, S. & Cuthbert, S., Elsevier, pp. 77-111、2011.
  • Naemura, K., Hirajima, T. and Svojtka, M., The pressure-temperature path and the origin of phlogopite in spinel-garnet peridotites from the Blansky les massif of the Moldanubian zone, Czech Repblic, Journal of Petrology, Oxford University Press, 50, pp. 1795-1827, 2009.
  • Naemura, K., Hisashima, H., Hirajima, T. and Svojtka, M., An ultra-high-pressure metamorphic condition and isothermal decompression path obtained from a garnet pyroxenite in the Horni Bory granulite of the Bohemian Massif , Journal of Mineralogical and Petrological Sciences, Japan association of Mineral Sciences, 104, pp. 168-175, 2009.
  • Naemura, K., Yokoyama, K., Hirajima, T. and Svojtka, M., Age determination of thorianite in phlogopite-bearing spinel-garnet peridotite in the Gfohl Unit, Moldanubian Zone of the Bohemian Massif, Journal of Mineralogical and Petrological Sciences, Japan association of Mineral Sciences, 103, pp. 285-290, 2008.
  • Nakamura, D., Svojtka, M., Naemura, K. and Hirajima, T., Very high-pressure (>4 GPa) eclogite associated with the Moldanubian Zone garnet peridotite (Nove Dvory, Czech Republic) , Journal of metamorphic geology, Wiley-Blackwell, 22, pp. 593-603, 2004.

総説論文(査読あり)

  • 苗村康輔、中村大輔、平島崇男、超高圧変成帯中のザクロ石橄欖岩およびエクロジャイトの温度圧力履歴解析法:地質温度計の概説と適用、岩石鉱物科学、41、pp. 225-246, 2012年 (日本語).
  • 杨建军、黄梦曦、苗村康辅、关于造山带幔源橄榄岩变质演化的一个普遍规律?、岩石学报(Acta Petrologica Sinica)、26、pp. 1479-1485, 2013年 (中国語).

紀要など(査読なし)

  • Naemura, K., Shibata, T. & Hirajima, T., Major element compositions of Mg-Cr rich garnet-bearing peridotites in the Moldanubian zone of the Bohemian Massif, 京都大学地球熱学研究施設紀要, pp. 33-36, 2009.

学会発表(岩手大学赴任以降のみ記載)

  • 苗村康輔、西田裕志、木下周祐、平島 崇男、清水 以知子、神居古潭変成帯・幌加内地域の泥質変成岩へのラマン炭質物温度計の適用、日本鉱物科学会2022年年会、9月、新潟大学