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DCフィールド | 値 | 言語 |
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dc.contributor.author | 見野, 和夫 | ja |
dc.contributor.author | 竹内, 文朗 | ja |
dc.contributor.alternative | MINO, Kazuo | en |
dc.contributor.alternative | TAKEUCHI, Fumiaki | en |
dc.date.accessioned | 2009-02-10T01:43:22Z | - |
dc.date.available | 2009-02-10T01:43:22Z | - |
dc.date.issued | 1977-04-01 | - |
dc.identifier.issn | 0386-412X | - |
dc.identifier.uri | http://hdl.handle.net/2433/70136 | - |
dc.description.abstract | A γ-ray survey was carried out using a handy type scintillation survey meter around theOhbaku fault, where the under ground structure had been made clear by seismic explorationand gravity survey.Six traversal lines were chosen to cross the fault. Most distinguishable peak of the γ-rayintensity appeared on the observation point M 59, midst of the main line. This peak seemsto be caused by the high content of radon in the fault zone.Maximum peak in each of the six traverses located almost in a straight line, from NW toSE, and this must be the strike of the Ohbaku fault. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | jpn | - |
dc.publisher | 京都大学防災研究所 | ja |
dc.publisher.alternative | Disaster Prevention Research Institute, Kyoto University | en |
dc.subject.ndc | 453.3 | - |
dc.subject.ndc | 454.4 | - |
dc.subject.ndc | 429.4 | - |
dc.title | 黄檗断層付近のγ線測定 | ja |
dc.title.alternative | γ-RAY SURVEY AROUND THE OHBAKU FAULT | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AN00027784 | - |
dc.identifier.jtitle | 京都大学防災研究所年報. B | ja |
dc.identifier.volume | 20 | - |
dc.identifier.issue | B-1 | - |
dc.identifier.spage | 29 | - |
dc.identifier.epage | 33 | - |
dc.textversion | publisher | - |
dc.sortkey | 04 | - |
dc.relation.url | http://www.dpri.kyoto-u.ac.jp/nenpo/nenpo.html | - |
dcterms.accessRights | open access | - |
dc.identifier.pissn | 0386-412X | - |
dc.identifier.jtitle-alternative | Disaster Prevention Research Institute Annuals. B | en |
出現コレクション: | No.20 B-1 |
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