@article{oai:ir.kagoshima-u.ac.jp:00011616,
 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 大石, 一久 and OISHI, Kazuhisa and 市村, 高男 and ICHIMURA, Takao},
 journal = {鹿児島大学理学部紀要, Reports of the Faculty of Science, Kagoshima University},
 month = {},
 note = {More than thirty-five Satsuma stone pagodas are known in the northwestern and southern parts of Kyushu. It was reported recently that Satsuma stone pagodas were made of massive tuff “Meiyuanshistone”of the Cretaceous Fangyan Formation distributed in the Ningbo area, China. Meiyuanshi-stone tuff is characterized by light reddish purple color and having the principal phenocrysts of quartz and albite. Rock samples were collected from the two Satsuma stone pagodas and a Sou-fu Shishi（Chinese stone statue of lion）, which are preserved in Hirado City, Nagasaki, Umi town, Fukuoka and Minami-kyushu City, Kagoshima. 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 all samples are almost same each other and the data are in agreement with one of Meiyuanshistone. Two Xiaoxishi-stone were also collected from a quarry at Ningbo, China and minerals of them were also identified by the same analyses. These analytical data are also in agreement with one of Meiyuanshistone, but Xiaoxishi-stone differs from Meiyuanshi-stone in having lamina generally.},
 pages = {9--24},
 title = {薩摩塔石材と中国寧波市の下部白亜系方岩組地層との対比},
 volume = {46},
 year = {2013}
}