{"_buckets": {"deposit": "038b0e10-4da5-44fc-b8f9-2cb7348e9f57"}, "_deposit": {"id": "33528", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33528"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033528", "sets": []}, "author_link": ["130971", "130970"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "\u6d25\u6ce2\u306e\u6ce2\u6e90\u57df\u306b\u304a\u3051\u308b\u6d77\u5e95\u5730\u5f62\u3068\u5909\u52d5"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1967-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "1464", "bibliographicPageStart": "1449", "bibliographicVolumeNumber": "44", "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": "Tsunami sources for the Kanto Earthquake of 1923, and the Boso-oki Earthquake of 1953 are estimated by means of an inverse refraction diagram. The former includes the whole of the elevated region at Miura and Boso Peninsula, the latter being located in the region which corresponds to the area of aftershock activity. The estimated source areas of tsunamis which were generated in the adjacent sea to Japan, are drawn on a bathymetric chart. The mean slope of the sea bottom in the vicinity of each source was of the order of 1/100\uff5e1/10. Tsunami energy seems to be affected by the slope of the sea bottom as well as the water depth at the source. The amount of the sea bottom deformation was estimated from the distribution of the inundation height of a tsunami along the coast. The average vertical displacement in the tsunami source is calculated by using the tsunami energy and the source area. The values thus obtained were of the order of several meters for large earthquakes.", "subitem_description_type": "Abstract"}, {"subitem_description": "1933\u5e74\u306e\u4e09\u9678\u6d25\u6ce2\u306b\u3064\u3044\u3066,\u5bae\u90e8(1934)\u306f\u5404\u5730\u306e\u691c\u6f6e\u8a18\u9320\u3092\u3082\u3068\u306b,\u6d25\u6ce2\u306e\u9006\u4f1d\u64ad\u56f3\u3092\u3048\u304c\u304d,\u6ce2\u6e90\u57df\u3092\u63a8\u5b9a\u3057\u305f.\u3053\u306e\u7d50\u679c,\u6ce2\u6e90\u306f\u304b\u306a\u308a\u5e83\u3044\u9818\u57df\u3092\u3082\u3064\u305f\u3053\u3068\u304c\u660e\u3089\u304b\u306b\u3055\u308c\u305f.\u4ee5\u6765,\u591a\u304f\u306e\u4eba\u9054\u306b\u3088\u3064\u3066,\u540c\u69d8\u306a\u65b9\u6cd5\u3067,\u4e8c\u5341\u6570\u500b\u306e\u6d25\u6ce2\u306e\u6539\u6e90\u57df\u304c\u63a8\u5b9a\u3055\u308c\u3066\u304d\u3066\u3044\u308b.\u4eca\u56de, 1923\u5e74\u306e\u95a2\u6771\u5730\u9707\u304a\u3088\u30731953\u5e74\u306e\u623f\u7dcf\u6c96\u5730\u9707\u306b\u4f34\u306a\u3064\u305f\u6d25\u6ce2\u306e\u6ce2\u6e90\u57df\u3092\u9006\u4f1d\u64ad\u56f3\u306b\u3088\u3064\u3066\u63a8\u5b9a\u3057\u305f\u3068\u3053\u308d,\u305d\u306e\u9577\u5f84\u306f\u305d\u308c\u305e\u308c\u7d04170km\u304a\u3088\u3073160km\u3067\u3042\u308b.\u307e\u305f\u95a2\u6771\u5730\u9707\u306e\u5834\u5408,\u305d\u306e\u6ce2\u6e90\u57df\u306f\u4e09\u6d66\u534a\u5cf6\u304a\u3088\u3073\u623f\u7dcf\u534a\u5cf6\u306e\u9686\u8d77\u5730\u5e2f\u3092\u5927\u304d\u304f\u5305\u542b\u3057,\u623f\u7dcf\u6c96\u5730\u9707\u306e\u6ce2\u6e90\u57df\u306f,\u305d\u306e\u4f59\u9707\u57df\u3068\u304b\u306a\u308a\u3088\u304f\u4e00\u81f4\u3057\u3066\u3044\u308b.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "130971", "nameIdentifierScheme": "WEKO"}], "names": 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