{"created":"2021-03-01T06:54:00.640410+00:00","id":35043,"links":{},"metadata":{"_buckets":{"deposit":"e57f9500-544c-43d1-833f-89c83fafe49e"},"_deposit":{"id":"35043","owner":"1","owners":[],"pid":{"revision_id":0,"type":"depid","value":"35043"},"status":"published"},"_oai":{"id":"oai:repository.dl.itc.u-tokyo.ac.jp:00035043","sets":["80:4535:5277","9:504:4538:5278"]},"author_link":["135151","135150"],"item_4_alternative_title_1":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Physiographic History of the Oku-Tango Peninsula"}]},"item_4_biblio_info_7":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1928-08-24","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"121","bibliographicPageStart":"111","bibliographicVolumeNumber":"5","bibliographic_titles":[{"bibliographic_title":"東京帝國大學地震研究所彙報 = Bulletin of the Earthquake Research Institute, Tokyo Imperial University"}]}]},"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 Oku-Tango Peninsula makes a two-cycled mountainland from the standpoint of its physiographic history. Low relief of its central plateau represents the cycle of erosion of the former age and maturely dissected hills along its margin show that of the present time. The characteristic of the present cycle is the occurrence of blocking movements, by which the surface of the former cycle has been uplifted to the present altitude and has formed the major tectonic feature of the peninsula. There are two types of fault in this region: one running from northwest to southeast, the other from northeast to southwest. Blocking movements in the present cycle have taken place neither continuously nor simultaneously, but have made a series of intermittent occurrences. Among them, latest three minor ones are distinctly observable in the topography of the peninsula. The first is a differential upheaval which is well explained by coastal terraces, the second, a slight submergence known from the shoreline of rias type, and the third, a tilting of land blocks represented by the recent Oku-Tango earthquake on March 7, 1927. In these minor episodes, we have found that the movements have been carried on always in the same sense, namely, blocks of land have been tilted up in their southeastern or northeastern side.","subitem_description_type":"Abstract"}]},"item_4_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"135151","nameIdentifierScheme":"WEKO"}],"names":[{"name":"多田, 文男"}]}]},"item_4_identifier_registration":{"attribute_name":"ID登録","attribute_value_mlt":[{"subitem_identifier_reg_text":"10.15083/0000035043","subitem_identifier_reg_type":"JaLC"}]},"item_4_publisher_20":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"東京帝国大学地震研究所"}]},"item_4_source_id_10":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00029699","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, Tokyo Imperial University"}]},"item_4_text_4":{"attribute_name":"著者所属","attribute_value_mlt":[{"subitem_text_value":"地震研究所"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"Tada, Fumio"}],"nameIdentifiers":[{"nameIdentifier":"135150","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":"ji0050009.pdf","filesize":[{"value":"695.8 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"ji0050009.pdf","url":"https://repository.dl.itc.u-tokyo.ac.jp/record/35043/files/ji0050009.pdf"},"version_id":"3383261a-d687-4801-a1b2-43d881e98649"}]},"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":"奥丹後半島の地形発達史","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"奥丹後半島の地形発達史","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"1","path":["5277","5278"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2008-06-06"},"publish_date":"2008-06-06","publish_status":"0","recid":"35043","relation_version_is_last":true,"title":["奥丹後半島の地形発達史"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2022-12-19T04:09:50.956283+00:00"}