{"created":"2023-06-19T10:35:14.361887+00:00","id":1188,"links":{},"metadata":{"_buckets":{"deposit":"c6833e54-c6f2-4d87-a99f-a0bc53690132"},"_deposit":{"created_by":14,"id":"1188","owners":[14],"pid":{"revision_id":0,"type":"depid","value":"1188"},"status":"published"},"_oai":{"id":"oai:ous.repo.nii.ac.jp:00001188","sets":["296:314:330"]},"author_link":[],"item_1_biblio_info_14":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1997-03-31","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"91","bibliographicPageStart":"81","bibliographicVolumeNumber":"32","bibliographic_titles":[{"bibliographic_title":"岡山理科大学紀要. A, 自然科学","bibliographic_titleLang":"ja"},{"bibliographic_title":"Bulletin of Okayama University of Science. A, Natural Sciences","bibliographic_titleLang":"en"}]}]},"item_1_creator_6":{"attribute_name":"著者名","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"坂本, 尚史","creatorNameLang":"ja"},{"creatorName":"サカモト, タカブミ","creatorNameLang":"ja-Kana"},{"creatorName":"Sakamoto, Takabumi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"小林, 祥一","creatorNameLang":"ja"},{"creatorName":"コバヤシ, ショウイチ","creatorNameLang":"ja-Kana"},{"creatorName":"Kobayashi, Shouichi","creatorNameLang":"en"}]}]},"item_1_description_1":{"attribute_name":"ページ属性","attribute_value_mlt":[{"subitem_description":"P(論文)","subitem_description_type":"Other"}]},"item_1_description_12":{"attribute_name":"抄録(英)","attribute_value_mlt":[{"subitem_description":"The constituent clay minerals of the weathered granites (saprolite), veins, and fractures in the Sanyo-type granitic body, and the vein in the Ryoke-type granitic body of Kitagi Island, Okayama Prefecture, have been examined by X-ray powder diffraction. The saprolite contains halloysite, vermiculite, and a small amount of kaolinite. The clay vein mainly consists of halloysite and a small amount of kaolinite, vermiculite, and di-octahedral smectite in the Sanyo-type granite, and kaolinite and vermiculite in the Ryoke-type granite. In the fracture, commonest clay mineral is di-octahedral smectite with subordinate amounts of halloysite and kaolinite. Mica clay mineral is found in all cases. The clay minerals in the saprolite were formed during the chemical weathering. On the other hand, it seems that the clay minerals in the veins and fractures are hydrothermal origin and remain unchanged through weathering.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_1_source_id_13":{"attribute_name":"雑誌書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AN00033244","subitem_source_identifier_type":"NCID"}]},"item_1_text_10":{"attribute_name":"著者所属(英)","attribute_value_mlt":[{"subitem_text_language":"en","subitem_text_value":"Department of Applied Science, Faculty of Science, Okayama University of Science"},{"subitem_text_language":"en","subitem_text_value":"Division of Earth Sciences, Kurashiki University of Science and the Arts"}]},"item_1_text_9":{"attribute_name":"著者所属(日)","attribute_value_mlt":[{"subitem_text_language":"ja","subitem_text_value":"岡山理科大学理学部基礎理学科"},{"subitem_text_language":"ja","subitem_text_value":"倉敷芸術科学大学産業科学技術学部機能物質学科"}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"1997-03-31"}],"displaytype":"detail","filename":"KJ00000063697.pdf","filesize":[{"value":"536.6 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"url":"https://ous.repo.nii.ac.jp/record/1188/files/KJ00000063697.pdf"},"version_id":"d62ce4be-83d4-40f8-a7e2-6e6b5f1bb242"}]},"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":"岡山県南部の風化花崗岩中の粘土鉱物 : その1:笠岡市北木島について","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"岡山県南部の風化花崗岩中の粘土鉱物 : その1:笠岡市北木島について","subitem_title_language":"ja"},{"subitem_title":"Clay Minerals in the Weathered Granitic Rocks in the Southern Part of Okayama Prefecture, Japan : Part 1. Its Mineralogy and Occurrence in Kitagi Island","subitem_title_language":"en"},{"subitem_title":"オカヤマケン ナンブ ノ フウカ カコウガン チュウ ノ ネンド コウブツソノ1 カサオカシ キタギジマ ニ ツイテ","subitem_title_language":"ja-Kana"}]},"item_type_id":"1","owner":"14","path":["330"],"pubdate":{"attribute_name":"PubDate","attribute_value":"1997-03-31"},"publish_date":"1997-03-31","publish_status":"0","recid":"1188","relation_version_is_last":true,"title":["岡山県南部の風化花崗岩中の粘土鉱物 : その1:笠岡市北木島について"],"weko_creator_id":"14","weko_shared_id":-1},"updated":"2023-09-28T00:55:22.058000+00:00"}