@article{oai:ous.repo.nii.ac.jp:00000568,
 author = {小林, 祥一 and Kobayashi, Shoichi and 三宅, 寛 and Miyake, Hiroshi},
 journal = {岡山理科大学紀要, The Bulletin of the Okayama University of Science,},
 month = {Mar},
 note = {P(論文), The basic～ultrabasic rocks mainly consisted of serpentinite comprising the rodingite were distributed at the Mt. Oosa in northern Okayama Prefecture. In particular, the rodingite masses were classified into two types according to their occurrence and mineral assemblage, and investigated microscopically as well as rontgenometrically in detail. The results obtained that difference of mineralogical constituents in the veinlets contained in the respective veins or masses of rodingite owing to their characteristic types. Between the rodingite masses from Oosa-cho and those from Singo-cho, Okayama Prefecture were characterized by some minerals. In addition, mineralogical studies of the veinlets in the basic～ultrabasic rocks except the rodingite described in the present paper.},
 pages = {79--88},
 title = {rodingiteの研究 第2報 : 岡山県大佐町における産状},
 volume = {14},
 year = {1979},
 yomi = {コバヤシ, ショウイチ and ミヤケ, ヒロシ}
}