{"_buckets": {"deposit": "3561b19b-f436-476b-a4c2-c538870183e5"}, "_deposit": {"id": "33652", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33652"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033652", "sets": []}, "author_link": ["131480", "131479"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "9. \u65b0\u6f5f\u5730\u9707\u306e\u6d25\u6ce2\u306b\u3064\u3044\u3066 : \u6d6a\u6e90\u304a\u3088\u3073\u4f1d\u64ad\u306e\u554f\u984c"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1965-07-15", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "148", "bibliographicPageStart": "129", "bibliographicVolumeNumber": "43", "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": "The distribution of inundation height along the coast near the tsunami source shows two peaks. This feature has close relation to the deformation of the sea bottom in the source area. From a refraction diagram, the initial crest-height at each station along the Japanese coast seems to follow Green\u0027s law. The distribution of tsunami energy seems to have been controlled by the submarine topography. The coast near the tsunami source seems to have received strong reflected waves from north Korea. As to other feature of propagation, long-waves propagated along the slope of the continental shelf seem to have existed. From several tide-gauge records, it was concluded that tsunami waves have uniformly decayed. Decay coefficient is approximately 0.043 per hour.", "subitem_description_type": "Abstract"}, {"subitem_description": "1964\u5e746\u670816\u65e513\u664202\u5206,\u65b0\u6f5f\u770c\u7c9f\u5cf6\u9644\u8fd1\u3067\u767a\u751f\u3057\u305f\u5730\u9707(\u6c17\u8c61\u5e81\u767a\u8868\u306b\u3088\u308c\u3070,\u9707\u592e\u306f38.4\u309cN,139.2\u00b0E,\u6df1\u305540km,\u30de\u30b0\u30cb\u30c1\u30e5\u30fc\u30c9\u7d047.7)\u306b\u4f34\u306a\u3064\u305f\u6d25\u6ce2\u306f,\u6d6a\u6e90\u9644\u8fd1\u306e\u6cbf\u5cb8\u3067\u6d25\u6ce2\u306e\u9ad8\u3055(M.S.L.\u4e0a)4\uff5e5m\u306b\u9054\u3057,\u5e83\u304f\u65e5\u672c\u6d77\u5168\u57df\u3067\u89b3\u6e2c\u3055\u308c\u305f.\u5404\u5730\u306e\u6982\u8981\u306fTable 1\u306b\u793a\u3059.\u3053\u306e\u6d25\u6ce2\u306e\u898f\u6a21\u306f1900\u5e74\u4ee5\u6765,\u65e5\u672c\u6d77\u306b\u767a\u751f\u3057\u305f4\u56de\u306e\u6d25\u6ce2\u306b\u6bd4\u3057\u6700\u5927\u3067,1833\u5e74(\u5929\u4fdd4\u5e74)\u306b\u4eca\u56de\u3068\u307b\u307c\u540c\u5730\u57df\u3067\u767a\u751f\u3057\u305f\u6d25\u6ce2\u306b\u5339\u6575\u3059\u308b.", "subitem_description_type": "Abstract"}]}, "item_4_full_name_3": {"attribute_name": "\u8457\u8005\u5225\u540d", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "131480", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "\u7fbd\u9ce5, \u5fb3\u592a\u90ce"}]}]}, "item_4_identifier_registration": {"attribute_name": "ID\u767b\u9332", "attribute_value_mlt": [{"subitem_identifier_reg_text": "10.15083/0000033652", "subitem_identifier_reg_type": "JaLC"}]}, "item_4_publisher_20": {"attribute_name": "\u51fa\u7248\u8005", "attribute_value_mlt": [{"subitem_publisher": "\u6771\u4eac\u5927\u5b66\u5730\u9707\u7814\u7a76\u6240"}]}, "item_4_source_id_10": {"attribute_name": "\u66f8\u8a8c\u30ec\u30b3\u30fc\u30c9ID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00162258", "subitem_source_identifier_type": "NCID"}]}, "item_4_source_id_8": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "00408972", "subitem_source_identifier_type": "ISSN"}]}, "item_4_subject_15": {"attribute_name": "\u65e5\u672c\u5341\u9032\u5206\u985e\u6cd5", "attribute_value_mlt": [{"subitem_subject": "453", "subitem_subject_scheme": "NDC"}]}, "item_4_text_21": {"attribute_name": "\u51fa\u7248\u8005\u5225\u540d", "attribute_value_mlt": [{"subitem_text_value": "Earthquake Research Institute, University of Tokyo"}]}, "item_4_text_34": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"subitem_text_value": "Departmental Bulletin Paper"}]}, "item_4_text_4": {"attribute_name": "\u8457\u8005\u6240\u5c5e", "attribute_value_mlt": [{"subitem_text_value": "Earthquake Research Institute"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "HATORI, Tokutaro"}], "nameIdentifiers": [{"nameIdentifier": "131479", "nameIdentifierScheme": "WEKO"}]}]}, "item_files": {"attribute_name": "\u30d5\u30a1\u30a4\u30eb\u60c5\u5831", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_date", "date": [{"dateType": "Available", "dateValue": "2017-06-26"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "ji0431009.pdf", "filesize": [{"value": "875.8 kB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 875800.0, "url": {"label": "ji0431009.pdf", "url": "https://repository.dl.itc.u-tokyo.ac.jp/record/33652/files/ji0431009.pdf"}, "version_id": "a0439d78-6373-4bb5-9e54-4a366a3d73ca"}]}, "item_language": {"attribute_name": "\u8a00\u8a9e", "attribute_value_mlt": [{"subitem_language": "eng"}]}, "item_resource_type": {"attribute_name": "\u8cc7\u6e90\u30bf\u30a4\u30d7", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_title": "9. On the Tsunami which accompanied the Niigata Earthquake of June 16, 1964. : Source Deformation, Propagation and Tsunami Run-up", "item_titles": {"attribute_name": "\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_title": "9. On the Tsunami which accompanied the Niigata Earthquake of June 16, 1964. : Source Deformation, Propagation and Tsunami Run-up", "subitem_title_language": "en"}]}, "item_type_id": "4", "owner": "1", "path": ["80/4535/4947/4955", "9/504/4538/4949/4956"], "permalink_uri": "https://doi.org/10.15083/0000033652", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2008-05-30"}, "publish_date": "2008-05-30", "publish_status": "0", "recid": "33652", "relation": {}, "relation_version_is_last": true, "title": ["9. On the Tsunami which accompanied the Niigata Earthquake of June 16, 1964. : Source Deformation, Propagation and Tsunami Run-up"], "weko_shared_id": -1}