@article{oai:ir.kagoshima-u.ac.jp:00010458,
 author = {大木, 公彦 and OKI, Kimihiko and 古澤, 明 and FURUSAWA, Akira and 高津, 孝 and TAKATSU, Takashi and 橋口, 亘 and HASHIGUCHI, Wataru and 内村, 公大 and UCHIMURA, Kimihiro},
 journal = {鹿児島大学理学部紀要, Reports of the Faculty of Science, Kagoshima University},
 month = {Nov},
 note = {More than twenty Satsuma stone pagodas are in the northwestern part of Kyushu. A Satsuma stone pagoda is preserved in the ruins of Ryufuku-ji temple, Ohmura City, Nagasaki Prefecture. Rock sample was collected from the Satsuma stone pagoda for comparison with the Satsuma stone pagoda of Bonotsu history museum “Kishinkan” and “Meiyuanshi-stone” collected from a quarry at Ningbo, China. Minerals of them were identified by X-ray diffractometer and chemical composition of feldspar was obtained by an energy dispersive X-ray micro-analyzer. These analytical data suggest that lithologic characters of the Satsuma stone pagoda from Ohmura City are equivalent to the latters. Furthermore rock samples of anchor stone preserved in Amami City and “Xiaoxi-stone” collected from Ningbo were analyzed by same methods. From these results it may be inferred that this anchor stone was quarried from the Fangyan Formation distributed in the Ningbo area, China.},
 pages = {1--15},
 title = {日本における薩摩塔・碇石の石材と中国寧波産石材の岩石学的特徴に関する一考察},
 volume = {43},
 year = {2010}
}