@article{oai:ir.kagoshima-u.ac.jp:00012590,
 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},
 journal = {鹿児島大学理学部紀要, Reports of the Faculty of Science, Kagoshima University},
 month = {},
 note = {The purpose of this study is to clarify the derivation of the Satsuma stone pagoda in Kagoshima Prefecture. Rock samples were collected from the Satsuma stone pagoda preserved in the Bonotsu history museum “Kishinkan” located in the southwestern part of Satsuma Peninsula, Kagoshima Prefecture and from a quarry at Ningbo, China. The latter sample is commonly called “Meiyuanshi-stone”. Chemical elements and their distribution were obtained by X-ray analytical microscope and minerals of them were identified by X-ray diffractometer. Furthermore, chemical composition of feldspar was obtained by an energy dispersive X-ray micro-analyzer. These analytical data suggest that lithologic characters of both rock samples are equivalent.},
 pages = {11--19},
 title = {薩摩塔石材と中国寧波産の梅園石との岩石学的分析による対比},
 volume = {42},
 year = {2009}
}