{"_buckets": {"deposit": "48aa6c1a-23ed-4461-a353-a34413455540"}, "_deposit": {"id": "32829", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32829"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032829", "sets": []}, "author_link": ["127843", "127842"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "Relation between Seismic Intensity near the Epicenter, Focal Depth and Magnitude"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1988-06-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "31", "bibliographicPageStart": "23", "bibliographicVolumeNumber": "63", "bibliographic_titles": [{"bibliographic_title": "\u6771\u4eac\u5927\u5b78\u5730\u9707\u7814\u7a76\u6240\u5f59\u5831 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]}, "item_4_description_13": {"attribute_name": "\u30d5\u30a9\u30fc\u30de\u30c3\u30c8", "attribute_value_mlt": [{"subitem_description": "application/pdf", "subitem_description_type": "Other"}]}, "item_4_description_5": {"attribute_name": "\u6284\u9332", "attribute_value_mlt": [{"subitem_description": "\u65e5\u672c\u306e\u5730\u9707\u306b\u3064\u3044\u3066,\u9707\u592e\u4ed8\u8fd1\u306e\u9707\u5ea6I0(\u6c17\u8c61\u5e81\u9707\u5ea6\u968e\u7d1a),\u30de\u30b0\u30cb\u30c1\u30e5\u30fc\u30c9M(\u6c17\u8c61\u5e81\u65b9\u5f0f),\u9707\u6e90\u306e\u6df1\u3055h(km)\u306e\u6a19\u6e96\u7684\u95a2\u4fc2\u3092\u8868\u3059\u5b9f\u9a13\u5f0f\u30921114\u500b\u306e\u9707\u5ea6\u30c7\u30fc\u30bf\u3092\u7528\u3044\u3066\u6c42\u3081,\u6b21\u5f0f\u3092\u5f97\u305f.M=0.23 I0+0.105 I02+1.2log h+1.3\u3053\u306e\u5f0f\u306fM\u304c2\uff5e8,h\u304cO\uff5e100km.I0\u304cO\uff5e6\u306e\u5730\u9707\u3092\u5bfe\u8c61\u3068\u3057\u3066\u3044\u308b.\u305f\u3060\u3057h=O\u3068\u767a\u8868\u3055\u308c\u3066\u3044\u308b\u5730\u9707\u306e\u5b9f\u969b\u306e\u6df1\u3055\u306f\u6570km\u3068\u8003\u3048\u3066,h\u003c3km\u306e\u5834\u5408\u306fh=3km\u3068\u7f6e\u304f,M\u304c5\u7a0b\u5ea6\u3088\u308a\u5927\u304d\u3044\u5730\u9707\u306b\u3064\u3044\u3066\u306fm=1.2I0+1.21log h-0.83\u3059\u306a\u308f\u3061I0=O.83 M-log h+0.71\u3092\u7528\u3044\u3066\u3082\u3088\u3044.", "subitem_description_type": "Abstract"}, {"subitem_description": "An empirical formula for the seismic intensity (JMA scale) I0 near the epicenter of an earthquake of magnitude M and focal depth h has been determined using 1114 data on seismic intensity recorded in Japan. The formula has the form M=0.23I0+O.105I02+1.2 log h+1.3 for M=2\uff5e8, h=3\uff5e100km, and I0\u22670. 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