| ID | 40188 |
| JaLCDOI | |
| Sort Key | 6
|
| Title Alternative | The isotopic ratio (234)U/(238)U of the ores and waters in Togo Mine, Tottori-ken, Japan
|
| FullText URL | |
| Author |
Umemoto, Shunji
|
| Abstract | 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.
|
| Note | 原著論文 (Original Paper)
|
| Publication Title |
岡山大学温泉研究所報告
|
| Published Date | 1967-12-15
|
| Volume | volume37
|
| Publisher | 岡山大学温泉研究所
|
| Publisher Alternative | Institute for Thermal Spring Research, Okayama University
|
| Start Page | 31
|
| End Page | 36
|
| ISSN | 0369-7142
|
| NCID | AN00032853
|
| Content Type |
Departmental Bulletin Paper
|
| OAI-PMH Set |
岡山大学
|
| language |
Japanese
|
| File Version | publisher
|
| NAID | |
| Eprints Journal Name | mmc
|
