{"created":"2023-07-27T06:20:20.011575+00:00","id":1529,"links":{},"metadata":{"_buckets":{"deposit":"841fd3d5-25d7-4413-8edd-d49fd32598b9"},"_deposit":{"created_by":3,"id":"1529","owners":[3],"pid":{"revision_id":0,"type":"depid","value":"1529"},"status":"published"},"_oai":{"id":"oai:kanazawa-u.repo.nii.ac.jp:00001529","sets":["11:25:49:56"]},"author_link":["4675"],"item_7_biblio_info_8":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1986-12-25","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"76","bibliographicPageStart":"58","bibliographicVolumeNumber":"3","bibliographic_titles":[{"bibliographic_title":"金沢大学文学部地理学報告"}]}]},"item_7_description_21":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"A morphometry of 225pyroclastic cones in Japan has been carried out with measurement using the topographic maps in 1:25,000scale. The results of the morphometry are Summarized as follows: (1) Most of scoria cones are 200-600 m wide and 20-100 m high and their craters are 100-300 m wide and 10-50 m deep. (2) The relative heights of the pyroclastic cones are less than 0.3 of the basal widths. (3) Most of the crater widths of the pyroclastic cones are more than a quarter of the basal widths. (4) Si0_2 values of the fragments composing the scoria cones are mostly less than 57%, and those of other pyroclastic cones range from 50 to 75%. (5) Proportions of basal widths to relative heights have no correlation to Si0_2 values. (6) Most of the pyroclastic cones in Japan have been formed since a few ten thousand years ago. (7) The scoria cones mainly distributed along the coast of the Sea of Japan and on Izu-Bonin arc. The tuff cones mainly stand along the volcanic front of Tohoku arc.","subitem_description_type":"Abstract"}]},"item_7_description_5":{"attribute_name":"提供者所属","attribute_value_mlt":[{"subitem_description":"金沢大学文学部地理学","subitem_description_type":"Other"}]},"item_7_source_id_11":{"attribute_name":"NCID","attribute_value_mlt":[{"subitem_source_identifier":"AN10063514","subitem_source_identifier_type":"NCID"}]},"item_7_source_id_9":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0289-789X","subitem_source_identifier_type":"ISSN"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"守屋, 以智雄"}],"nameIdentifiers":[{"nameIdentifier":"4675","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":"2017-10-02"}],"displaytype":"detail","filename":"KJ00004304555.pdf","filesize":[{"value":"1.1 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"KJ00004304555.pdf","url":"https://kanazawa-u.repo.nii.ac.jp/record/1529/files/KJ00004304555.pdf"},"version_id":"81934f07-3fac-49b5-90cc-d17e77f39058"}]},"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":"日本の火砕丘の地形計測","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"日本の火砕丘の地形計測"},{"subitem_title":"Morphometry of Pyroclastic Cones in Japan","subitem_title_language":"en"}]},"item_type_id":"7","owner":"3","path":["56"],"pubdate":{"attribute_name":"公開日","attribute_value":"2017-10-02"},"publish_date":"2017-10-02","publish_status":"0","recid":"1529","relation_version_is_last":true,"title":["日本の火砕丘の地形計測"],"weko_creator_id":"3","weko_shared_id":-1},"updated":"2023-07-28T04:08:22.616271+00:00"}