{"created":"2021-03-01T06:19:55.096449+00:00","id":16887,"links":{},"metadata":{"_buckets":{"deposit":"55344d15-4df7-4705-87d8-0b27c27b7516"},"_deposit":{"id":"16887","owners":[],"pid":{"revision_id":0,"type":"depid","value":"16887"},"status":"published"},"_oai":{"id":"oai:soar-ir.repo.nii.ac.jp:00016887","sets":["1628:1629:1652"]},"author_link":["48299","48300","48301","48302"],"item_11_biblio_info_6":{"attribute_name":"書誌情報","attribute_value_mlt":[{"bibliographicIssueDates":{"bibliographicIssueDate":"1993-03-31","bibliographicIssueDateType":"Issued"},"bibliographicPageEnd":"104","bibliographicPageStart":"99","bibliographicVolumeNumber":"15","bibliographic_titles":[{"bibliographic_title":"環境科学年報"}]}]},"item_11_description_20":{"attribute_name":"抄録","attribute_value_mlt":[{"subitem_description":":A uthors found the grayish white mudstone from the fresh outcrops at the site of land development in the east-side region of the .Fossa Magna，c entral Japan. Grayish white mudstones have been observed from view points of the occurence mode and morphologicai features. Its significance has been dicussed The grayish white mudstones have been identified as calcium carabonate by chemical analysis and X-ray microanalyzer. The calcarious mudstones have been found only in the Aoki formation for the surveyable part in the region. Calcium carbonate content was the range of 4 to 83 %. The formation of calcarious mudstone was about 0.1 to 60 cm thick. The morphological features of calcarious formation were mostly alayer type，a nd occasiortally ac oncave type，a r adical type，a w edge type，a l amina type，a nd al ode type. The grayish white mudstones have been found only on the deep horizon. It was then suggested that calcarious mudstones mitigate a acidification of soil by sulfuric acid which was derived from the oxidation of pyrite by the joint action of air and rain water","subitem_description_type":"Abstract"}]},"item_11_description_30":{"attribute_name":"資源タイプ（コンテンツの種類）","attribute_value_mlt":[{"subitem_description":"Article","subitem_description_type":"Other"}]},"item_11_description_5":{"attribute_name":"引用","attribute_value_mlt":[{"subitem_description":"環境科学年報15:99-104(1993)","subitem_description_type":"Other"}]},"item_11_link_3":{"attribute_name":"信州大学研究者総覧へのリンク","attribute_value_mlt":[{"subitem_link_text":"藤松, 仁","subitem_link_url":"http://soar-rd.shinshu-u.ac.jp/profile/ja.gCSNjekV.html"}]},"item_11_publisher_4":{"attribute_name":"出版者","attribute_value_mlt":[{"subitem_publisher":"信州大学環境科学研究会"}]},"item_11_source_id_35":{"attribute_name":"ISSN","attribute_value_mlt":[{"subitem_source_identifier":"0915-7492","subitem_source_identifier_type":"ISSN"}]},"item_11_source_id_40":{"attribute_name":"書誌レコードID","attribute_value_mlt":[{"subitem_source_identifier":"AN1054947X","subitem_source_identifier_type":"NCID"}]},"item_1627890728808":{"attribute_name":"出版タイプ","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":"矢彦沢,  清允"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"山本,  満寿夫"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"上野,  満夫"}],"nameIdentifiers":[{}]},{"creatorNames":[{"creatorName":"藤松,  仁"}],"nameIdentifiers":[{}]}]},"item_files":{"attribute_name":"ファイル情報","attribute_type":"file","attribute_value_mlt":[{"accessrole":"open_date","date":[{"dateType":"Available","dateValue":"2015-09-28"}],"displaytype":"detail","filename":"15-16.pdf","filesize":[{"value":"653.5 kB"}],"format":"application/pdf","licensetype":"license_note","mimetype":"application/pdf","url":{"label":"15-16.pdf","url":"https://soar-ir.repo.nii.ac.jp/record/16887/files/15-16.pdf"},"version_id":"1b1fefc8-2a14-484d-aedd-aea2a0845657"}]},"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":"research report","resourceuri":"http://purl.org/coar/resource_type/c_18ws"}]},"item_title":"フオツサマグナ東端地域に分布する第三系海成堆積物中に見出される石灰質泥岩とその意義","item_titles":{"attribute_name":"タイトル","attribute_value_mlt":[{"subitem_title":"フオツサマグナ東端地域に分布する第三系海成堆積物中に見出される石灰質泥岩とその意義","subitem_title_language":"ja"},{"subitem_title":"On the Calcareous Mudstones from Tertiary Marine Sediments in the east，-side region of the Fossa Magna, Central Japan, and its Significance","subitem_title_language":"en"}]},"item_type_id":"11","owner":"1","path":["1652"],"pubdate":{"attribute_name":"PubDate","attribute_value":"2011-04-19"},"publish_date":"2011-04-19","publish_status":"0","recid":"16887","relation_version_is_last":true,"title":["フオツサマグナ東端地域に分布する第三系海成堆積物中に見出される石灰質泥岩とその意義"],"weko_creator_id":"1","weko_shared_id":-1},"updated":"2023-01-18T01:56:44.698739+00:00"}