{"_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": ["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", "download_preview_message": "", "file_order": 0, "filename": "26-1-3.pdf", "filesize": [{"value": "6.7 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 6700000.0, "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"], "permalink_uri": "https://kitami-it.repo.nii.ac.jp/records/6720", "pubdate": {"attribute_name": "公開日", "attribute_value": "2007-04-09"}, "publish_date": "2007-04-09", "publish_status": "0", "recid": "6720", "relation": {}, "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_shared_id": 3}