{"_buckets": {"deposit": "24302b4f-f48b-4e8f-af88-f53390d60b92"}, "_deposit": {"id": "2006994", "owners": [1], "pid": {"revision_id": 0, "type": "depid", "value": "2006994"}, "status": "published"}, "_oai": {"id": "oai:u-ryukyu.repo.nii.ac.jp:02006994", "sets": ["1642838000887", "1642838406414"]}, "author_link": [], "item_1617186331708": {"attribute_name": "Title", "attribute_value_mlt": [{"subitem_1551255647225": "\u6c96\u7e04\u8fd1\u6d77\u306e\u77f3\u7070\u8cea\u6d77\u5e95\u6c88\u6bbf\u7269\u306e\u5316\u5b66\u6210\u5206\u3068\u7d50\u6676\u69cb\u9020", "subitem_1551255648112": "ja"}, {"subitem_1551255647225": "Geochemical Study on Marine Carbonate Sediments in OKINAWA", "subitem_1551255648112": "en"}]}, "item_1617186419668": {"attribute_name": "Creator", "attribute_type": "creator", "attribute_value_mlt": [{"creatorNames": [{"creatorName": "\u517c\u5cf6, \u6e05", "creatorNameLang": "ja"}]}, {"creatorNames": [{"creatorName": "\u6e21\u4e45\u5c71, \u7ae0", "creatorNameLang": "ja"}]}, {"creatorNames": [{"creatorName": "\u77e5\u540d, \u5b9a\u5247", "creatorNameLang": "ja"}]}, {"creatorNames": [{"creatorName": "Kaneshima, Kiyoshi", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "Tokuyama, Akira", "creatorNameLang": "en"}]}, {"creatorNames": [{"creatorName": "China, Sadanori", "creatorNameLang": "en"}]}]}, "item_1617186476635": {"attribute_name": "Access Rights", "attribute_value_mlt": [{"subitem_1522299639480": "open access", "subitem_1600958577026": "http://purl.org/coar/access_right/c_abf2"}]}, "item_1617186626617": {"attribute_name": "Description", "attribute_value_mlt": [{"subitem_description": "The geochemical studies and X-ray analysis were conducted on marine carbonate sediments obtained from off-shores of Okinawa Island. The conglomerate or massive carbonate sediments are composed of 46.7 per cent of CaO and 4.0 per cent of MgO. These sediments contain, as impurities, relatively large amounts of silica, iron, aluminum and phosphate comparing with those of Riukiu limestone. Positive correlations appear to exist between iron, aluminum and phosphate contents. The amount of sandy sediments diminish rapidly at the particle size near 65 meshes. The calcium carbonate content of sandy sediments also depend largely upon the particle size showing to positive correlation, wherease silicate and heavy minerals increase in fine powder sediments. The conglomerate or massive carbonate sediments are composed of high-magnesian-calcite, aragonite and quartz. The cose sandy sediments are composed of high-magnesian-calcite, aragonite, low-magnesian-calcite and quartz, whereas fine sandy sediments contain large amounts of silicate and heavy minerals.", "subitem_description_type": "Other"}, {"subitem_description": "\u7d00\u8981\u8ad6\u6587", "subitem_description_type": "Other"}]}, "item_1617186643794": {"attribute_name": "Publisher", "attribute_value_mlt": [{"subitem_1522300295150": "ja", "subitem_1522300316516": "\u7409\u7403\u5927\u5b66\u7406\u5de5\u5b66\u90e8"}, {"subitem_1522300295150": "en", "subitem_1522300316516": "Science and Engineering Division, University of the Ryukyus"}]}, "item_1617186702042": {"attribute_name": "Language", "attribute_value_mlt": [{"subitem_1551255818386": "jpn"}]}, "item_1617186783814": {"attribute_name": "Identifier", "attribute_value_mlt": [{"subitem_identifier_type": "HDL", "subitem_identifier_uri": "http://hdl.handle.net/20.500.12000/23539"}]}, "item_1617186941041": {"attribute_name": "Source Title", "attribute_value_mlt": [{"subitem_1522650068558": "ja", "subitem_1522650091861": "\u7409\u7403\u5927\u5b66\u7406\u5de5\u5b66\u90e8\u7d00\u8981. \u7406\u5b66\u7de8"}, {"subitem_1522650068558": "en", "subitem_1522650091861": "Bulletin of Science \u0026 Engineering Division, University of Ryukyus. Mathematics \u0026 natural sciences"}]}, "item_1617187056579": {"attribute_name": "Bibliographic Information", "attribute_value_mlt": [{"bibliographicIssueNumber": "22", "bibliographicPageEnd": "13", "bibliographicPageStart": "1"}]}, "item_1617258105262": {"attribute_name": "Resource Type", "attribute_value_mlt": [{"resourcetype": "departmental bulletin paper", "resourceuri": "http://purl.org/coar/resource_type/c_6501"}]}, "item_1617265215918": {"attribute_name": "Version Type", "attribute_value_mlt": [{"subitem_1522305645492": "NA", "subitem_1600292170262": "http://purl.org/coar/version/c_be7fb7dd8ff6fe43"}]}, "item_1617605131499": {"attribute_name": "File", "attribute_type": "file", "attribute_value_mlt": [{"accessrole": "open_access", "download_preview_message": "", "file_order": 0, "filename": "No22p001.pdf", "future_date_message": "", "is_thumbnail": false, "mimetype": "", "size": 0, "url": {"objectType": "fulltext", "url": "https://u-ryukyu.repo.nii.ac.jp/record/2006994/files/No22p001.pdf"}, "version_id": "7a158c1b-b7fe-432c-9331-80f0ddfd9b37"}]}, "item_title": "\u6c96\u7e04\u8fd1\u6d77\u306e\u77f3\u7070\u8cea\u6d77\u5e95\u6c88\u6bbf\u7269\u306e\u5316\u5b66\u6210\u5206\u3068\u7d50\u6676\u69cb\u9020", "item_type_id": "15", "owner": "1", "path": ["1642838000887", "1642838406414"], "permalink_uri": "http://hdl.handle.net/20.500.12000/23539", "pubdate": {"attribute_name": "PubDate", "attribute_value": "2012-02-28"}, "publish_date": "2012-02-28", "publish_status": "0", "recid": "2006994", "relation": {}, "relation_version_is_last": true, "title": ["\u6c96\u7e04\u8fd1\u6d77\u306e\u77f3\u7070\u8cea\u6d77\u5e95\u6c88\u6bbf\u7269\u306e\u5316\u5b66\u6210\u5206\u3068\u7d50\u6676\u69cb\u9020"], "weko_shared_id": -1}