{"created":"2021-03-01T06:52:19.421339+00:00","id":33532,"links":{},"metadata":{"_buckets":{"deposit":"8ca71101-32f4-4a39-ab7c-ef652727ac78"},"_deposit":{"id":"33532","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"33532"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00033532","sets":["80:4535:4937:4938","9:504:4538:4939:4940"]},"author_link":["130995","130994"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"地球熱学 第20報 : 山岳形成と熱伝導"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1967-03-31","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"4","bibliographicPageEnd":"1551","bibliographicPageStart":"1537","bibliographicVolumeNumber":"44","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":"Time-variations of temperature within a mountain range are calculated by applying the relaxation technique to solving an equation of thermal conduction in the following two-dimensional mountain models. 1) A mountain range which is formed by a rapid erosion. 2) Mountain formation is caused by water erosion, the speed of which is very slow and constant. 3) A volcanic intrusion penetrated a flat plain. The results of the computations indicate that an L-type isotherm pattern would not be actually observed in geothermal measurements provided the geologically accepted age of mountains is true. It is possible to roughly estimate the age of a volcanic dome if it is younger than a few 104 years. Mt. Minakamiyama, a volcanic dome in the central area of the Matsushiro Earthquake Swarm, seems to be older than 104 years, the conclusion being consistent with the result obtained by a K-Ar method.","subitem_description_type":"Abstract"},{"subitem_description":"山岳が浸蝕や火山活動によつて形成された後,温度分布が時間の経過とともに,どのように変化して行くかを,熱伝導方程式によつて計算した.山岳形成モデルとして 1) 断層・地すべりの類によつて急に形成された場合. 2) ゆるやかな浸蝕で形成されて来た場合. 3) 火山活動によつて形成された場合.を採用した.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"130995","nameIdentifierScheme":"WEKO"}],"names":[{"name":"萩原, 幸男"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000033532","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_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Hagiwara, Yukio"}],"nameIdentifiers":[{"nameIdentifier":"130994","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":"ji0444009.pdf","filesize":[{"value":"760.4 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0444009.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/33532/files/ji0444009.pdf"},"version_id":"bdf0f69b-17f4-406c-bc8a-d4d779df2fe3"}]},"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":"Studies of the Thermal State of the Earth The 20th Paper : Mountain Formation and Thermal Conduction","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"Studies of the Thermal State of the Earth The 20th Paper : Mountain Formation and Thermal Conduction","subitem_title_language":"en"}]},"item_type_id":"4","owner":"1","path":["4938","4940"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-05-30"},"publish_date":"2008-05-30","publish_status":"0","recid":"33532","relation_version_is_last":true,"title":["Studies of the Thermal State of the Earth The 20th Paper : Mountain Formation and Thermal Conduction"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:45:33.226806+00:00"}