{"_buckets": {"deposit": "ea23cebb-103b-4cd5-b786-6d5ba1a087d1"}, "_deposit": {"id": "32782", "owner": "1", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "32782"}, "status": "published"}, "_oai": {"id": "oai:repository.dl.itc.u-tokyo.ac.jp:00032782", "sets": []}, "author_link": ["127500", "127501", "127502", "127503", "127504", "127495", "127496", "127497", "127498", "127499"], "item_4_alternative_title_1": {"attribute_name": "\u305d\u306e\u4ed6\u306e\u30bf\u30a4\u30c8\u30eb", "attribute_value_mlt": [{"subitem_alternative_title": "DELP 1986\u5e74\u5ea6 \u5317\u897f\u592a\u5e73\u6d0b\u7814\u7a76\u822a\u6d77\u5831\u544a : Part II \u6d77\u6d0b\u5e95\u5730\u6bbb\u5730\u9707\u6ce2\u901f\u5ea6\u69cb\u9020"}]}, "item_4_biblio_info_7": {"attribute_name": "\u66f8\u8a8c\u60c5\u5831", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1990-06-30", "bibliographicIssueDateType": "Issued"}, "bibliographicIssueNumber": "1", "bibliographicPageEnd": "104", "bibliographicPageStart": "89", "bibliographicVolumeNumber": "65", "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 large scale seismic experiment was carried out in the northwestern Pacific Basin in 1986. Two long range profiles were shot using OBS\u0027s and explosives to investigate the nature of the lateral heterogeneity and anisotropy of an old oceanic lithosphere. An airgun array was also used as a controlled seismic source. Three airgun profiles were shot in order to obtain a detailed crustal structure of normal ocean type and to constrain the deeper structure obtained from the long range profiles. A seismic wavespeed model for both P and S waves is presented. The model seems adequate to represent the crust sampled over 700km distance. The model is in good areement with the model previously obtained near DSDP Hole 581C. However, our data do not substantiate the presence of LVZ in the lower crust.", "subitem_description_type": "Abstract"}, {"subitem_description": "1986\u5e74\u5317\u897f\u592a\u5e73\u6d0b\u6d77\u76c6\u306b\u304a\u3044\u3066\u5927\u898f\u6a21\u5730\u9707\u63a2\u67fb\u5b9f\u9a13\u304c\u884c\u306a\u308f\u308c\u305f. 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