ID | 40188 |
JaLCDOI | |
Sort Key | 6
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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
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フルテキストURL | |
著者 |
梅本 春次
岡山大学温泉研究所化学部門
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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.
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備考 | 原著論文 (Original Paper)
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出版物タイトル |
岡山大学温泉研究所報告
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発行日 | 1967-12-15
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巻 | 37巻
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出版者 | 岡山大学温泉研究所
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出版者(別表記) | Institute for Thermal Spring Research, Okayama University
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開始ページ | 31
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終了ページ | 36
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ISSN | 0369-7142
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NCID | AN00032853
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資料タイプ |
紀要論文
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OAI-PMH Set |
岡山大学
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言語 |
日本語
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論文のバージョン | publisher
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NAID | |
Eprints Journal Name | mmc
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