WEKO3
アイテム
{"_buckets": {"deposit": "3a9c79cc-659c-4bad-974c-ca1d2c8fcfbb"}, "_deposit": {"id": "28199", "owners": [], "pid": {"revision_id": 0, "type": "depid", "value": "28199"}, "status": "published"}, "_oai": {"id": "oai:niigata-u.repo.nii.ac.jp:00028199", "sets": ["456", "1579"]}, "item_7_alternative_title_1": {"attribute_name": "その他のタイトル", "attribute_value_mlt": [{"subitem_alternative_title": "A Proposal for the prediction of hazardous landslide areas"}]}, "item_7_biblio_info_6": {"attribute_name": "書誌情報", "attribute_value_mlt": [{"bibliographicIssueDates": {"bibliographicIssueDate": "1982-11", "bibliographicIssueDateType": "Issued"}, "bibliographicPageEnd": "64", "bibliographicPageStart": "51", "bibliographicVolumeNumber": "4", "bibliographic_titles": [{"bibliographic_title": "新潟大学積雪地域災害研究センター研究年報"}, {"bibliographic_title": "新潟大学積雪地域災害研究センター研究年報", "bibliographic_titleLang": "en"}]}]}, "item_7_description_4": {"attribute_name": "抄録", "attribute_value_mlt": [{"subitem_description": "The result of the study on the Mushigame landslide which occurred in 1980 can be summarized as following lines (FUJITA, Y. et al 1981); 1. The sliding plane near main scarp has developed not within the bed rock of Miocene Shiiya formation, but in the older landslide debris deposit. 2. The normal faults (lunar fault crack) have developed in this older debris mostly behind the crown of the main scarp. These faults have been formed prior to the sIiding (Fig. 2). 3. The older debris deposits might fall down along these faults and the landslide was brought about in succession (Photo. 1). 4. Before sliding, we can frequently recognized the graben-like small valley behind the scarp. Those features are also recognized at the other recently sliding areas such as the Nigorisawa, Kamibanba, Nakamaruke in Niigata Prefecture and Showa-mura and Yamato-machi in Fukushima Prefecture. Therefore, we emphasize the importance of discovery of above-mentioned features; namely fault, or crack, graben in landslide areas, for prediction of hazardous sliding area. Figure 10 shows a hazard map in Yamakoshi-mura, from the above-mentioned standpoint.", "subitem_description_type": "Abstract"}]}, "item_7_full_name_3": {"attribute_name": "著者別名", "attribute_value_mlt": [{"nameIdentifiers": [{"nameIdentifier": "162058", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Fujita, Yukinori"}]}, {"nameIdentifiers": [{"nameIdentifier": "162059", "nameIdentifierScheme": "WEKO"}], "names": [{"name": "Aoki, Shigeru"}]}]}, "item_7_publisher_7": {"attribute_name": "出版者", "attribute_value_mlt": [{"subitem_publisher": "新潟大学積雪地域災害研究センター"}]}, "item_7_select_19": {"attribute_name": "著者版フラグ", "attribute_value_mlt": [{"subitem_select_item": "publisher"}]}, "item_7_source_id_11": {"attribute_name": "書誌レコードID", "attribute_value_mlt": [{"subitem_source_identifier": "AN00183327", "subitem_source_identifier_type": "NCID"}]}, "item_7_source_id_9": {"attribute_name": "ISSN", "attribute_value_mlt": [{"subitem_source_identifier": "03877892", "subitem_source_identifier_type": "ISSN"}]}, "item_creator": {"attribute_name": "著者", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "藤田, 至則"}], "nameIdentifiers": [{"nameIdentifier": "162056", "nameIdentifierScheme": "WEKO"}]}, {"creatorNames": [{"creatorName": "青木, 滋"}], "nameIdentifiers": [{"nameIdentifier": "162057", "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": "2019-08-20"}], "displaytype": "detail", "download_preview_message": "", "file_order": 0, "filename": "4_51-64.pdf", "filesize": [{"value": "1.4 MB"}], "format": "application/pdf", "future_date_message": "", "is_thumbnail": false, "licensetype": "license_free", "mimetype": "application/pdf", "size": 1400000.0, "url": {"label": "4_51-64.pdf", "url": "https://niigata-u.repo.nii.ac.jp/record/28199/files/4_51-64.pdf"}, "version_id": "26fc5447-08ce-4960-b3ff-5932cd5b3f6d"}]}, "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": "地すべり予測に関する基礎的研究", "item_titles": {"attribute_name": "タイトル", "attribute_value_mlt": [{"subitem_title": "地すべり予測に関する基礎的研究"}, {"subitem_title": "地すべり予測に関する基礎的研究", "subitem_title_language": "en"}]}, "item_type_id": "7", "owner": "1", "path": ["456", "1579"], "permalink_uri": "http://hdl.handle.net/10191/39011", "pubdate": {"attribute_name": "公開日", "attribute_value": "2016-03-03"}, "publish_date": "2016-03-03", "publish_status": "0", "recid": "28199", "relation": {}, "relation_version_is_last": true, "title": ["地すべり予測に関する基礎的研究"], "weko_shared_id": null}
地すべり予測に関する基礎的研究
http://hdl.handle.net/10191/39011
http://hdl.handle.net/10191/390110ab2653a-f250-4f53-82ab-5697c9e0813f
名前 / ファイル | ライセンス | アクション |
---|---|---|
![]() |
|
Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
---|---|---|---|---|---|---|
公開日 | 2016-03-03 | |||||
タイトル | ||||||
タイトル | 地すべり予測に関する基礎的研究 | |||||
タイトル | ||||||
言語 | en | |||||
タイトル | 地すべり予測に関する基礎的研究 | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
その他のタイトル | ||||||
その他のタイトル | A Proposal for the prediction of hazardous landslide areas | |||||
著者 |
藤田, 至則
× 藤田, 至則× 青木, 滋 |
|||||
著者別名 | ||||||
識別子 | 162058 | |||||
識別子Scheme | WEKO | |||||
姓名 | Fujita, Yukinori | |||||
著者別名 | ||||||
識別子 | 162059 | |||||
識別子Scheme | WEKO | |||||
姓名 | Aoki, Shigeru | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The result of the study on the Mushigame landslide which occurred in 1980 can be summarized as following lines (FUJITA, Y. et al 1981); 1. The sliding plane near main scarp has developed not within the bed rock of Miocene Shiiya formation, but in the older landslide debris deposit. 2. The normal faults (lunar fault crack) have developed in this older debris mostly behind the crown of the main scarp. These faults have been formed prior to the sIiding (Fig. 2). 3. The older debris deposits might fall down along these faults and the landslide was brought about in succession (Photo. 1). 4. Before sliding, we can frequently recognized the graben-like small valley behind the scarp. Those features are also recognized at the other recently sliding areas such as the Nigorisawa, Kamibanba, Nakamaruke in Niigata Prefecture and Showa-mura and Yamato-machi in Fukushima Prefecture. Therefore, we emphasize the importance of discovery of above-mentioned features; namely fault, or crack, graben in landslide areas, for prediction of hazardous sliding area. Figure 10 shows a hazard map in Yamakoshi-mura, from the above-mentioned standpoint. | |||||
書誌情報 |
新潟大学積雪地域災害研究センター研究年報 en : 新潟大学積雪地域災害研究センター研究年報 巻 4, p. 51-64, 発行日 1982-11 |
|||||
出版者 | ||||||
出版者 | 新潟大学積雪地域災害研究センター | |||||
ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 03877892 | |||||
書誌レコードID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AN00183327 | |||||
著者版フラグ | ||||||
値 | publisher |