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ID 40188
フルテキストURL
タイトル(別表記)
The isotopic ratio (234)U/(238)U of the ores and waters in Togo Mine, Tottori-ken, Japan
著者
梅本 春次 岡山大学温泉研究所化学部門
抄録
The ratio (234)U/(238)U of two groups of ores and the waters collected in Kannokura Deposit was determined by α-ray spectrometry. According to the geological and mineralogical observation, the ores of each group were formed in succession. Based on the assumption that (234)U/(238)U of the uranium in the leaching solution is higher than that in the ores, the obtained ratio supports the above mechanism of formation. Actually, the waters collected in Kannokura Deposit showed the fairly high value in (234)U/(238)U. Each stratum of a typical section of the mine was observed on the ratio, but the obtained values were in too much complicated relation to interpret.
備考
原著論文 (Original Paper)
発行日
1967-12-15
出版物タイトル
岡山大学温泉研究所報告
出版物タイトル(別表記)
Papers of the Institute for Thermal Spring Research, Okayama University
37巻
出版者
岡山大学温泉研究所
出版者(別表記)
Institute for Thermal Spring Research, Okayama University
開始ページ
31
終了ページ
36
ISSN
0369-7142
NCID
AN00032853
資料タイプ
紀要論文
言語
Japanese
OAI-PMH Set
岡山大学
論文のバージョン
publisher
査読
無し
Sort Key
6
Eprints Journal Name
mmc