{"created":"2021-03-01T06:51:17.721458+00:00","id":32606,"links":{},"metadata":{"_buckets":{"deposit":"93a45fb3-a03d-4660-82b8-5f036dc5865a"},"_deposit":{"id":"32606","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"32606"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00032606","sets":["80:4535:4639:4643","9:504:4538:4641:4644"]},"author_link":["126166","126165"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"結晶内安定同位体比塁帯構造による岩石中の地殻内流通動通路\"\"みずみち\"\"の証拠"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2002-02-12","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"331","bibliographicPageStart":"321","bibliographicVolumeNumber":"76","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":"The crustal fluid conduit (Mizu-michi) contains large displacements of brittle rocks caused by faults and fractures during crustal movements. Mizu-michi is confirmed as veins, altered zones on a macro-scale, and grain-boundaries on a micro-scale. Macro- and micro-scale stable isotope studies are carried out from outcrops to grain-boundary scale in different types of crustal rock. The combination of carbon and oxygen isotopic analyses provided important constrains on the origin and the transportation mechanism of crustal fluid, mainly composed of carbon(C)-hydrogen (H)-oxygen (O) fluid during crustal movements. Isotopic data also provide evidence of the evolution of the crustal fluids on a molecular scale, accompanying an isotope-exchange mechanism involving fluids and minerals, and have major implications for micro fracture-controlled fluid-flow processes in the deep Earth's crust.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"126166","nameIdentifierScheme":"WEKO"}],"names":[{"name":"和田, 秀樹"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000032606","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":"458","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":"Department of Bilology and Geosciences, Shizuoka University"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Wada, Hideki"}],"nameIdentifiers":[{"nameIdentifier":"126165","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":"ji0763005.pdf","filesize":[{"value":"1.5 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0763005.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/32606/files/ji0763005.pdf"},"version_id":"44bd2db4-ec9d-4eea-a936-3b7fbfde9bb2"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"carbon isotope","subitem_subject_scheme":"Other"},{"subitem_subject":"oxygen isotope","subitem_subject_scheme":"Other"},{"subitem_subject":"isotopic zonation","subitem_subject_scheme":"Other"},{"subitem_subject":"Mizu-michi","subitem_subject_scheme":"Other"},{"subitem_subject":"crustal fluid","subitem_subject_scheme":"Other"}]},"item_language":{"attribute_name":"言語","attribute_value_mlt":[{"subitem_language":"eng"}]},"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":"Evidence of Crustal Fluid Flow Conduit (Mizu-michi) in Rocks by Stable Isotopic Zonation of Minerals","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Evidence of Crustal Fluid Flow Conduit (Mizu-michi) in Rocks by Stable Isotopic Zonation of Minerals","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4643","4644"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"32606","relation_version_is_last":true,"title":["Evidence of Crustal Fluid Flow Conduit (Mizu-michi) in Rocks by Stable Isotopic Zonation of Minerals"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:08:37.209528+00:00"}