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.
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.