{"_buckets": {"deposit": "30216707-5f57-4234-b03d-208dedc36811"}, "_deposit": {"id": "33489", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "33489"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00033489"}, "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "1966\u5e74Argo\u53f7\u306b\u3088\u308b\u897f\u592a\u5e73\u6d0b\u5730\u78c1\u6c17\u6e2c\u91cf\u7d50\u679c\u53ca\u3073\u540c\u5730\u57df\u306e\u78c1\u6c17\u5206\u5e03\u56f3"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1967-11-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "3", "bibliographicPageEnd": "814", "bibliographicPageStart": "799", "bibliographicVolumeNumber": "45", "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": "A total force geomagnetic survey was made in the northwestern Pacific during the US-Japan Scientific Cooperation Cruise of the R/V Argo of the Scripps Institution of Oceanography. In this survey, eleven seamounts were surveyed in detail both magnetically and bathymetrically. Combined with the existing data taken previously by both Japanese and US researchers, revised charts of the total geomagnetic field and its anomaly have been drawn for the area west of 172\u00b0E between 24\u00b0N and 46\u00b0N. The existence of magnetic lineations trending SWW-NEE which were noted previously have been confirmed, and their extension has been noted. They generally disappear as they get closer to the coast, but some seem to penetrate into the Japan Trench area. In the Shikoku Basin, the linear anomalies do not seem to exist. Some magnetic anomaly profiles have been investigated to see if there is any correlation with the anomalies in the Eastern and Central Pacific area. For a definite conclusion, however, good profiles in NNW-SSE direction in the northern Pacific area between 160\u00b0E and 180\u00b0E would be needed.", "subitem_description_type": "Abstract"}, {"subitem_description": 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and Geophysical Institute, University of Tokyo."}, {"subitem_text_value": "Scripps Institution of Oceanography, Marine Physical Laboratory, University of California"}, {"subitem_text_value": "Maizuru Marine Observatory, Japan Meteorological Agency."}, {"subitem_text_value": "Hydrographic Department,"}]}, "item_creator": {"attribute_name": "\u8457\u8005", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "Uyeda, S"}], "nameIdentifiers": [{"nameIdentifier": "130776", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Vacquier, V."}], "nameIdentifiers": [{"nameIdentifier": "130777", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Yasui, M."}], "nameIdentifiers": [{"nameIdentifier": "130778", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Sclater, J."}], "nameIdentifiers": [{"nameIdentifier": "130779", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "Sato, T."}], 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