{"_buckets": {"deposit": "9de857ee-0bd4-406b-8149-0e5f3227206d"}, "_deposit": {"id": "32835", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32835"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032835", "sets": []}, "author_link": ["127903", "127904", "127905", "127906", "127907", "127908", "127909", "127896", "127897", "127898", "127899", "127900", "127901", "127902"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "DELP 1985\u5e74\u5ea6\u65e5\u672c\u6d77\u7814\u7a76\u822a\u6d77\u5831\u544a : V. \u5730\u6bbb\u71b1\u6d41\u91cf\u6e2c\u5b9a"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1988-03-31", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "4", "bibliographicPageEnd": "432", "bibliographicPageStart": "417", "bibliographicVolumeNumber": "62", "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": "Heat flow measurements were carried out in the Japan Sea at three stations on the KH82-4 cruise of R/V Hakuho-Maru and twelve stations on the DELP-85 WAKASHIO cruise. In the Yamato Basin, heat flow is very uniform and consistent with the existing data. The ages of the Yamato Basin and Tsushima Basin are estimated to be about 25 m.y. if based on the heat flow data. It was proved that the heat flow is variable in the Mogami Trough which was previously thought to be a low heat flow zone. A high heat flow value possibly associated with an anomalous reflector was obtained in the hypocentral region of the 1983 Nihonkai-Chubu Earthquake.", "subitem_description_type": "Abstract"}, {"subitem_description": 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