{"created":"2021-03-01T06:51:21.973312+00:00","id":32670,"links":{},"metadata":{"_buckets":{"deposit":"e137666a-7cd2-4d0d-bf41-678161339201"},"_deposit":{"id":"32670","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32670"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032670","sets":["80:4535:4665:4666","9:504:4538:4667:4668"]},"author_link":["126700","126701","126702","126703","126696","126697","126698","126699"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Effect of the Latent Heat on the Gas- hydrate/Gas Phase Boundary Depth Due to the  Faulting"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1999-03-29","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3-4","bibliographicPageEnd":"317","bibliographicPageStart":"305","bibliographicVolumeNumber":"73","bibliographic_titles":[{"bibliographic_title":"東京大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, University of Tokyo"}]}]},"item_4_description_13":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_5":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"BSRs, often observed at the Nankai accretionary complex, are considered to coincide with the base of the methane gas hydrate stability field (BGHS). The absence of BSR was discovered along the deep-tow multi-channel survey track, which can result because the insitu P-T condition is still in a transient state after fault activity. We conducted a two-dimensional numerical simulation of the thermal regime after faulting to simulate the time variation of BGHS depth. The latent heat due to formation/dissociation of gas hydrate has a significant effect on the thermal regime. The time constant for re-equilibration of the phase transition depth is ca 10 to several tens of years, which is longer by one order of magnitude for the case with latent heat considered than for the case with latent heat ignored.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"126700","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Kinoshita, Masataka"}]},{"nameIdentifiers":[{"nameIdentifier":"126701","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Nakano, Yukihiko"}]},{"nameIdentifiers":[{"nameIdentifier":"126702","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Goto, Shusaku"}]},{"nameIdentifiers":[{"nameIdentifier":"126703","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Ashi, Juichiro"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032670","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","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":"日本十進分類法","attribute_value_mlt":[{"subitem_subject":"453","subitem_subject_scheme":"NDC"}]},"item_4_text_21":{"attribute_name":"出版者別名","attribute_value_mlt":[{"subitem_text_value":"Earthquake Research Institute, University of Tokyo"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"東海大学海洋学部"},{"subitem_text_value":"東京大学大学院理学系研究科"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"木下, 正高"}],"nameIdentifiers":[{"nameIdentifier":"126696","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"中野, 幸彦"}],"nameIdentifiers":[{"nameIdentifier":"126697","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"後藤, 秀作"}],"nameIdentifiers":[{"nameIdentifier":"126698","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"芦, 寿一郎"}],"nameIdentifiers":[{"nameIdentifier":"126699","nameIdentifierScheme":"WEKO"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2017-06-26"}],"displaytype":"detail","filename":"ji0733004.pdf","filesize":[{"value":"1.3 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0733004.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32670/files/ji0733004.pdf"},"version_id":"2a361c8a-335b-443e-b113-fd6faa17bba8"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"gas hydrate","subitem_subject_scheme":"Other"},{"subitem_subject":"BSR","subitem_subject_scheme":"Other"},{"subitem_subject":"Nankai Trough","subitem_subject_scheme":"Other"},{"subitem_subject":"heat flow","subitem_subject_scheme":"Other"},{"subitem_subject":"latent heat","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"jpn"}]},"item_resource_type":{"attribute_name":"資源タイプ","attribute_value_mlt":[{"resourcetype":"departmental bulletin paper","resourceuri":"http://purl.org/coar/resource_type/c_6501"}]},"item_title":"断層運動に伴うガスハイドレート下面深度の変化に及ぼす潜熱の影響","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"断層運動に伴うガスハイドレート下面深度の変化に及ぼす潜熱の影響","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["4666","4668"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"32670","relation_version_is_last":true,"title":["断層運動に伴うガスハイドレート下面深度の変化に及ぼす潜熱の影響"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T05:17:20.767526+00:00"}