{"created":"2021-03-01T06:52:40.538215+00:00","id":33846,"links":{},"metadata":{"_buckets":{"deposit":"ba6f84c2-280b-40a8-b2e3-19af2d45e0a1"},"_deposit":{"id":"33846","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33846"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033846","sets":["80:4535:4997:5001","9:504:4538:4999:5002"]},"author_link":["132063","132064","132061","132062"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"26.地球熱学(第6報)秋田県院内油田,および,関東地方三地点における地殻熱流量"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1960-07-10","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"3","bibliographicPageEnd":"436","bibliographicPageStart":"421","bibliographicVolumeNumber":"38","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":"Values of terrestrial heat flow have been determined at four localities in Honshu, the Main Island of Japan, for deep wells penetrating sedimentary layers. The sedimentary strata being saturated with water in situ, thermal conductivity of the cores was measured in the saturated state. The heat flow values are, each in the unit of 10-6 cal/cm2sec, 1.49 at Innai Oil Field, Akita Prefecture, 0.74 at Tokyo University, Tokyo, 0.76 at Kashima, Ibaraki Pref. and 0.91 at Katsuta, Ibaraki Pref. As far as the eastern part of Japan is concerned, the data so far obtained seem to suggest that the heat flow is smaller on the Pacific coast side than inland and on the Japan Sea side. Repeated temperature measurements in the wells at Kashima and Katsuta showed that the temperature data obtained immediately after the end of boring are not correct except near the bottom.|第五報に報告したように,堆積岩の熱伝道度は,水による飽和状態において最大値を有する.油田,ガス田等の深井では,地層は,飽和状態にあると考えられるので,そのような場所での地殻熱流量の推定には上記の最大熱伝導度が用いられるべきである.このような考えに従つて,本州内四地点での地殻熱流量をもとめた.結果は,秋田県院内油田において1.49×10-6 cal/cm2sec,東京大学において0.74×10-8 cal/cm-sec,次数県鹿島において0.76×10-6 cal/cm-sec,および同県勝田において0.91×10-6 cal/cm2secである.従来得られた結果と照合すると,東北日本に関する限り,太平洋側では,地殻熱流量は,世界的平均より更に低いようである.更に測点を増し,この傾向を確かめることが望まれる.また,ボーリングに伴う地中温度の擾乱の程度,およびこの擾乱の恢復について有用な測定が,鹿島,勝田のガス井について行なわれた.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"132063","nameIdentifierScheme":"WEKO"}],"names":[{"name":"上田, 誠也"}]},{"nameIdentifiers":[{"nameIdentifier":"132064","nameIdentifierScheme":"WEKO"}],"names":[{"name":"宝来, 帰一"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033846","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":"Earthquake Research Institute"},{"subitem_text_value":"Graduate School, University of Tokyo"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Uyeda, Seiya"}],"nameIdentifiers":[{"nameIdentifier":"132061","nameIdentifierScheme":"WEKO"}]},{"creatorNames":[{"creatorName":"Horai, Ki-iti"}],"nameIdentifiers":[{"nameIdentifier":"132062","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":"2017-06-27"}],"displaytype":"detail","filename":"ji0383005.pdf","filesize":[{"value":"848.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0383005.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33846/files/ji0383005.pdf"},"version_id":"427d3b29-ef8c-41f9-b0d0-4f1dca77cb3e"}]},"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":"26. Studies of the Thermal State of the Earth : The Sixth Paper: Terrestrial Heat Flow at Innai Oil Field, Akita Prefecture and at Three Localities in Kanto-District, Japan","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"26. Studies of the Thermal State of the Earth : The Sixth Paper: Terrestrial Heat Flow at Innai Oil Field, Akita Prefecture and at Three Localities in Kanto-District, Japan","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["5001","5002"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"33846","relation_version_is_last":true,"title":["26. Studies of the Thermal State of the Earth : The Sixth Paper: Terrestrial Heat Flow at Innai Oil Field, Akita Prefecture and at Three Localities in Kanto-District, Japan"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:58:08.205239+00:00"}