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ファイル | 記述 | サイズ | フォーマット | |
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sgk01000_127.pdf | 617.9 kB | Adobe PDF | 見る/開く |
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DCフィールド | 値 | 言語 |
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dc.contributor.author | OZAWA, Izuo | en |
dc.date.accessioned | 2013-09-02T04:25:00Z | - |
dc.date.available | 2013-09-02T04:25:00Z | - |
dc.date.issued | 1970-12 | - |
dc.identifier.issn | 0454-7837 | - |
dc.identifier.uri | http://hdl.handle.net/2433/178577 | - |
dc.description.abstract | The abrupt changes of the crustal strains during the earthquakes have been observed with some components of highly sensitive extensometers. The relations between the seismic magnitude M and the coefficient k of the transmission of the abrupt change have been obtained as log k=1.17M+4.52, Moreover, the relations between the magnitude M and those of the radius of the fault area r_0 and the total released energy of the crustal strain Er have been calculated as, log r_0=0.45M+3.00, log Er=l.3M+13.4. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | Geophysical Institute, Kyoto University | en |
dc.subject.ndc | 450 | - |
dc.title | OBSERVATIONS OF ABRUPT CHANGES OF CRUSTAL STRAINS DURING EARTHQUAKES | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AA00423961 | - |
dc.identifier.jtitle | Special Contributions of the Geophysical Institute, Kyoto University | en |
dc.identifier.volume | 10 | - |
dc.identifier.spage | 127 | - |
dc.identifier.epage | 136 | - |
dc.textversion | publisher | - |
dc.sortkey | 13 | - |
dcterms.accessRights | open access | - |
dc.identifier.pissn | 0454-7837 | - |
出現コレクション: | No.10 |

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