{"created":"2023-07-25T08:11:25.434610+00:00","id":11616,"links":{},"metadata":{"_buckets":{"deposit":"309c27dc-43d7-48db-a84a-3745be899cef"},"_deposit":{"created_by":18,"id":"11616","owners":[18],"pid":{"revision_id":0,"type":"depid","value":"11616"},"status":"published"},"_oai":{"id":"oai:ir.kagoshima-u.ac.jp:00011616","sets":["228:229:5067","37:53"]},"author_link":[],"item_7_biblio_info_5":{"attribute_name":"収録雑誌名","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"2013","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"24","bibliographicPageStart":"9","bibliographicVolumeNumber":"46","bibliographic_titles":[{"bibliographic_title":"鹿児島大学理学部紀要","bibliographic_titleLang":"ja"},{"bibliographic_title":"Reports of the Faculty of Science, Kagoshima University","bibliographic_titleLang":"en"}]}]},"item_7_date_6":{"attribute_name":"作成日","attribute_value_mlt":[{"subitem_date_issued_datetime":"2013-12-30","subitem_date_issued_type":"Collected"}]},"item_7_description_4":{"attribute_name":"要約(Abstract)","attribute_value_mlt":[{"subitem_description":"More than thirty-five Satsuma stone pagodas are known in the northwestern and southern parts of Kyushu. It was reported recently that Satsuma stone pagodas were made of massive tuff “Meiyuanshistone”of the Cretaceous Fangyan Formation distributed in the Ningbo area, China. Meiyuanshi-stone tuff is characterized by light reddish purple color and having the principal phenocrysts of quartz and albite. Rock samples were collected from the two Satsuma stone pagodas and a Sou-fu Shishi（Chinese stone statue of lion）, which are preserved in Hirado City, Nagasaki, Umi town, Fukuoka and Minami-kyushu City, Kagoshima. Minerals of them were identified by X-ray diffractometer and chemical composition of feldspar was obtained by an energy dispersive X-ray micro-analyzer. These analytical data suggest that lithologic characters of all samples are almost same each other and the data are in agreement with one of Meiyuanshistone. Two Xiaoxishi-stone were also collected from a quarry at Ningbo, China and minerals of them were also identified by the same analyses. These analytical data are also in agreement with one of Meiyuanshistone, but Xiaoxishi-stone differs from Meiyuanshi-stone in having lamina generally.","subitem_description_language":"en","subitem_description_type":"Other"}]},"item_7_publisher_23":{"attribute_name":"公開者・出版者","attribute_value_mlt":[{"subitem_publisher":"鹿児島大学","subitem_publisher_language":"ja"},{"subitem_publisher":"Kagoshima University","subitem_publisher_language":"en"}]},"item_7_source_id_7":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"13456938","subitem_source_identifier_type":"PISSN"}]},"item_7_source_id_9":{"attribute_name":"NII書誌ID","attribute_value_mlt":[{"subitem_source_identifier":"AA11246904","subitem_source_identifier_type":"NCID"}]},"item_7_subject_15":{"attribute_name":"NDC","attribute_value_mlt":[{"subitem_subject":"458","subitem_subject_scheme":"NDC"}]},"item_7_version_type_14":{"attribute_name":"著者版フラグ","attribute_value_mlt":[{"subitem_version_resource":"http://purl.org/coar/version/c_970fb48d4fbd8a85","subitem_version_type":"VoR"}]},"item_creator":{"attribute_name":"著者","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"大木, 公彦","creatorNameLang":"ja"},{"creatorName":"OKI, Kimihiko","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"古澤, 明","creatorNameLang":"ja"},{"creatorName":"FURUSAWA, Akira","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"高津, 孝","creatorNameLang":"ja"},{"creatorName":"TAKATSU, Takashi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"橋口, 亘","creatorNameLang":"ja"},{"creatorName":"HASHIGUCHI, Wataru","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"大石, 一久","creatorNameLang":"ja"},{"creatorName":"OISHI, Kazuhisa","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"市村, 高男","creatorNameLang":"ja"},{"creatorName":"ICHIMURA, Takao","creatorNameLang":"en"}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2016-10-31"}],"displaytype":"detail","filename":"A critical comparison of stones of Satsuma stone pagoda.pdf","filesize":[{"value":"1.6 MB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"A critical comparison of stones of Satsuma stone pagoda.pdf","objectType":"fulltext","url":"https://ir.kagoshima-u.ac.jp/record/11616/files/A critical comparison of stones of Satsuma stone pagoda.pdf"},"version_id":"70e7fb83-28f5-4f2f-bceb-eea40f733454"}]},"item_keyword":{"attribute_name":"キーワード","attribute_value_mlt":[{"subitem_subject":"Satsuma stone pagoda","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"mineral composition","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Meiyuanshi-stone","subitem_subject_language":"en","subitem_subject_scheme":"Other"},{"subitem_subject":"Ningbo","subitem_subject_language":"en","subitem_subject_scheme":"Other"}]},"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":"薩摩塔石材と中国寧波市の下部白亜系方岩組地層との対比","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"薩摩塔石材と中国寧波市の下部白亜系方岩組地層との対比","subitem_title_language":"ja"},{"subitem_title":"A critical comparison of stones of Satsuma stone pagoda and rocks of the lower Cretaceous Fangyan Formation in Ningbo, China","subitem_title_language":"en"}]},"item_type_id":"7","owner":"18","path":["53","5067"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2014-03-07"},"publish_date":"2014-03-07","publish_status":"0","recid":"11616","relation_version_is_last":true,"title":["薩摩塔石材と中国寧波市の下部白亜系方岩組地層との対比"],"weko_creator_id":"18","weko_shared_id":-1},"updated":"2024-02-08T04:50:02.982933+00:00"}