{"created":"2023-06-19T11:36:11.546857+00:00","id":3057,"links":{},"metadata":{"_buckets":{"deposit":"9d270e88-91cd-4632-b4ec-8c1063eb6768"},"_deposit":{"created_by":13,"id":"3057","owners":[13],"pid":{"revision_id":0,"type":"depid","value":"3057"},"status":"published"},"_oai":{"id":"oai:mie-u.repo.nii.ac.jp:00003057","sets":["143:144:234:251"]},"author_link":["37705","37706","37707"],"item_4_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1994-03-10","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"61","bibliographicPageStart":"45","bibliographicVolumeNumber":"45","bibliographic_titles":[{"bibliographic_title":"三重大学教育学部研究紀要. 自然科学"}]}]},"item_4_description_14":{"attribute_name":"フォーマット","attribute_value_mlt":[{"subitem_description":"application/pdf","subitem_description_type":"Other"}]},"item_4_description_4":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":"Systematic field and laboratory studies of the profile of the Nakayama fire-clay mine and its surrounding deposits (Kiko, Daidō, Moyama and Shinmeito) in the northeastern part of Toki city, show these genetic relation with the underlying basement rock of Meso and/or Paleozoic and Miocene formation. The writers also have carried out the field observation of geological occurrence of the \"Kibushi\" clay and mineralogical studies of xonstitute materials and some experiments of hydraulic elutration for clay are examined. In Nakayama deposit, clay formation can be classified into the following three zone: sandy clay zone, \"Kibushi\" clay zone and bed rock. Further \"Kibushi\" clay zone is divided into three sub-zones. Whereas, two \"Kibushi\" clay sub-zones occurred in the profile at the Daido and Moyama mines. General trend of paleo-topography of masement in this area tends to gently incline toward the west, based on the sedimentation of \"Kibushi\" clay zones. Most of sandy clay and \"Kibushi\" clay are composed mainly of kaoline, and fine-grained quartz and feldspar. Small amount of sericite are included in some sandy clay. In Nakayama mine, clay zones contain a small amounts of montmorillonite but hardly to recognize it in other mine. Numerous massive marcasite nodules occur in the lower zone of \"KIbushi\" clay in Nakayama mine. Also small weathered dolomite masses are included in sandy zone in Moyama mine.@@@わが国の代表的な耐火粘土鉱床として古くから知られる、東海地方での、木節粘土の産地の1つである岐阜県土岐市中山陶土鉱山およびその周辺の基幸・大洞・茂山・新明陶鉱山の鉱床形態および構成鉱物の産状、性状について述べる。この地域の陶土層（土岐口累層）は主として中・古生層を基盤とする複雑な形状の凹地に堆積したもので、全般に砂質粘土が優位であり、数枚の亜炭層を挾む木節粘土層が中山鉱床では3層準分布する。本地域は基盤の古地形や陶土層の堆積状況から鉱床胚胎の谷は緩やかに西に下がっており、また構成粘土鉱物の性状などからも本陶土層は東側の風化砕屑物が運ばれて堆積したと思われる。大洞・茂山鉱床のプロファイルは下位から砂質粘土層、木節粘土層（2層ないし1層）、砂礫層からなり、おもな構成鉱物はカオリナイト、石英で、一部にセリサイトを伴う。モンモリロナイトは中山鉱床の陶土層中に普遍的に含まれるが、この両鉱床では見られない。中山鉱床の下位木節粘土層の一部から、マーカサイトノジュールが多数産する。また鉱山によって多数のドロマイト塊を含む砂質粘土層や小さなギブサイトボールを数多く含む層を胚胎する砂質粘土層が分布する。","subitem_description_type":"Abstract"}]},"item_4_publisher_30":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"三重大学教育学部"}]},"item_4_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0389-9225","subitem_source_identifier_type":"PISSN"}]},"item_4_source_id_9":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN00234199","subitem_source_identifier_type":"NCID"}]},"item_4_text_18":{"attribute_name":"その他のタイトル","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Mineralogical studies on the occurrence of Nakayama fire-clay mine, Toki, Gifu Prefecture"}]},"item_4_text_65":{"attribute_name":"資源タイプ（三重大）","attribute_value_mlt":[{"subitem_text_value":"Departmental Bulletin Paper / 紀要論文"}]},"item_access_right":{"attribute_name":"アクセス権","attribute_value_mlt":[{"subitem_access_right":"metadata only access","subitem_access_right_uri":"http://purl.org/coar/access_right/c_14cb"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"小倉, 義雄","creatorNameLang":"ja"},{"creatorName":"Ogura, Yoshio","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"垣下, 智","creatorNameLang":"ja"},{"creatorName":"Kakishita, Satoshi","creatorNameLang":"en"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"下坂, 康哉","creatorNameLang":"ja"},{"creatorName":"Shimosaka, Koya","creatorNameLang":"en"}],"nameIdentifiers":[{}]}]},"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":"岐阜県土岐市中山陶土鉱山地域の鉱床および構成鉱物の性状について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"岐阜県土岐市中山陶土鉱山地域の鉱床および構成鉱物の性状について","subitem_title_language":"ja"}]},"item_type_id":"4","owner":"13","path":["251"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2018-03-16"},"publish_date":"2018-03-16","publish_status":"0","recid":"3057","relation_version_is_last":true,"title":["岐阜県土岐市中山陶土鉱山地域の鉱床および構成鉱物の性状について"],"weko_creator_id":"13","weko_shared_id":-1},"updated":"2023-11-07T05:08:50.755222+00:00"}