{"created":"2021-03-01T06:52:43.567048+00:00","id":33891,"links":{},"metadata":{"_buckets":{"deposit":"eb24a092-359f-4233-b2f4-d136ef2e6af4"},"_deposit":{"id":"33891","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33891"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033891","sets":["80:4535:5007:5013","9:504:4538:5009:5014"]},"author_link":["132187","132186"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"On the Accuracy of Hypocentre Determination 3"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1959-08-25","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"2","bibliographicPageEnd":"345","bibliographicPageStart":"337","bibliographicVolumeNumber":"37","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"At 12h 00m, June 15, 1958, 156 tons of explosives were fired in Gifu Prefecture, central part of Japan, in order to obtain rocks for the construction of Mihoro dam. The seismic waves generated by this blast were recorded at about 10 observatories under the Japan Meteorological Agency. Although the recorded amplitude was rather small and the onset of initial motion was not clear except at Matsushiro, the attempt to determine the quantities concerning hypocentre was done by the method of least squares. The results which are given in Table 2 confirmed my previous conclusions. In the present calculation the position of epicentre was determined within 0.1 degree, the velocity was determined rather well, but the determination of the origin time is not good. Giving weight to the observation at Matsushiro we could obtain better results, especially with respect to the origin time. The velocity of