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b15p3n099p14.pdf | 224.44 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 | HASHIZUME, Michio | en |
dc.contributor.author | OIKE, Kazuo | en |
dc.contributor.author | KISHIMOTO, Yoshimichi | en |
dc.date.accessioned | 2010-09-08T07:55:49Z | - |
dc.date.available | 2010-09-08T07:55:49Z | - |
dc.date.issued | 1966-03-19 | - |
dc.identifier.issn | 0454-7675 | - |
dc.identifier.uri | http://hdl.handle.net/2433/124708 | - |
dc.description.abstract | Observation of microearthquakes in the western part of Kinki District has been carried out at 5 stations attached to the Tottori Microearthquake Observatory. Epicenters of about 200 earthquakes for ten months since Angust, 1964 were determined, giving a particular pattern of distribution. The areas in which the earthquakes occur frequently are separated in a complicated but nevertheless sharp manner from the areas where earthquakes seldom occur. Magnitude of these earthquakes was distributed from -1 up to more than 4. The distribution of direction of the first P motion shows a definite pattern for almost all earthquakes. This pattern coincides well with that of earthquakes with larger magnitude in this district. | en |
dc.format.mimetype | application/pdf | - |
dc.language.iso | eng | - |
dc.publisher | Disaster Prevention Research Institute, Kyoto University | en |
dc.title | Investigation of Microearthquakes in Kinki District -Seismicity and mechanism of their occurrence- | en |
dc.type | departmental bulletin paper | - |
dc.type.niitype | Departmental Bulletin Paper | - |
dc.identifier.ncid | AA00581033 | - |
dc.identifier.jtitle | Bulletin of the Disaster Prevention Research Institute | en |
dc.identifier.volume | 15 | - |
dc.identifier.issue | 3 | - |
dc.identifier.spage | 35 | - |
dc.identifier.epage | 47 | - |
dc.textversion | publisher | - |
dc.sortkey | 05 | - |
dcterms.accessRights | open access | - |
出現コレクション: | Vol.15 Pt.3 |

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