{"created":"2021-03-01T05:59:09.599359+00:00","id":6720,"links":{},"metadata":{"_buckets":{"deposit":"2220ee2a-ab34-4046-9662-21d343bf118a"},"_deposit":{"id":"6720","owners":[],"pid":{"revision_id":0,"type":"depid","value":"6720"},"status":"published"},"_oai":{"id":"oai:kitami-it.repo.nii.ac.jp:00006720","sets":["7:15:47"]},"item_2_alternative_title_18":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_alternative_title":"Characteristics　of　large-scale　landslides　in　the　Shiretoko　Peninsula，Eastern Hokkaido，Japan."}]},"item_2_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1994-09","bibliographicIssueDateType":"Issued"},"bibliographicIssueNumber":"1","bibliographicPageEnd":"28","bibliographicPageStart":"15","bibliographicVolumeNumber":"26","bibliographic_titles":[{"bibliographic_title":"北見工業大学研究報告"}]}]},"item_2_description_14":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_2_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"The Shiretoko Peninsula in eastern Hokkaido is known for its abundance of landslides.　In this region，a total of 606 landslides were identified in aerial photographs of which 97 were large-scale landslides (more than 500 m wide or 20 ha in area). The characteristics of large-scale landslides in the Shiretoko Peninsula are summarized as follows :  1)Large-scale landslides are mostly found along the margins of Pliocene to Quaternary subaerial andesitic lavas overlying Miocene volcaniclastic and clastic rocks. One of the geological factors for large-scale landslides is cap rock structures composed of subaerial lavas and underlying Miocene strata， which are susceptible to small-scale landsliding.  2)Most large-scale landslides are of rock-slump-type shape or debris-avalanche-type shape，the latter of which is characterized by a main scarp with large relative elevation, sliding mass under the scarp, and sliding/flowing debris of several hundreds meters in length. Moreover，also recognized were debris flows forming the waste-filled valleys of 400 to 500 meters wide and 3 to 4 kilometers long. 3) Moving and depositional areas in large-scale landslides were mostly enlarged by the repeated occurrence of landslides and flows of sliding mass， and the new sliding occured on the back-slope of the main scarp. 4)In order to understand the mechanism of large-scale sliding， the relationships of the Rausudake active faults and the destruction of the dome-like volcaro to the Onnebetsudake large-scale landslides should be further investigated in detail.","subitem_description_type":"Abstract"}]},"item_2_full_name_3":{"attribute_name":"著者別名","attribute_value_mlt":[{"nameIdentifiers":[{"nameIdentifier":"33885","nameIdentifierScheme":"WEKO"}],"names":[{"name":"Yoji, ITO"}]}]},"item_2_publisher_32":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"北見工業大学"}]},"item_2_select_15":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_select_item":"publisher"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"伊藤, 陽司"}],"nameIdentifiers":[{"nameIdentifier":"33884","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":"2016-11-22"}],"displaytype":"detail","filename":"26-1-3.pdf","filesize":[{"value":"6.7 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"26-1-3.pdf","url":"https://kitami-it.repo.nii.ac.jp/record/6720/files/26-1-3.pdf"},"version_id":"a1d0acfc-bb82-4c4a-bd64-65c532318d6e"}]},"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":"北海道東部，知床半島における大規模地すべり・崩壊地形の特徴","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"北海道東部，知床半島における大規模地すべり・崩壊地形の特徴"}]},"item_type_id":"2","owner":"1","path":["47"],"pubdate":{"attribute_name":"公開日","attribute_value":"2007-04-09"},"publish_date":"2007-04-09","publish_status":"0","recid":"6720","relation_version_is_last":true,"title":["北海道東部，知床半島における大規模地すべり・崩壊地形の特徴"],"weko_creator_id":"1","weko_shared_id":3},"updated":"2022-12-13T02:20:04.023458+00:00"}