{"created":"2022-02-24T07:11:16.169798+00:00","id":2017692,"links":{},"metadata":{"_buckets":{"deposit":"bade5389-be55-448d-9f92-059acf46c8e1"},"_deposit":{"created_by":14,"id":"2017692","owners":[14],"pid":{"revision_id":0,"type":"depid","value":"2017692"},"status":"published"},"_oai":{"id":"oai:u-ryukyu.repo.nii.ac.jp:02017692","sets":["1642838163960:1645772410074:1645675744155:1645675975519","1642838403551:1642838412624"]},"author_link":[],"item_1617186331708":{"attribute_name":"Title","attribute_value_mlt":[{"subitem_1551255647225":"[研究ノート] 沖縄の第四紀琉球石灰岩に分布する円錐カルストに関する研究","subitem_1551255648112":"ja"},{"subitem_1551255647225":"[Reserch note] A Study of Cone Karsts Developed on Quaternary Ryukyu Limestone in Okinawa","subitem_1551255648112":"en"}]},"item_1617186419668":{"attribute_name":"Creator","attribute_type":"creator","attribute_value_mlt":[{"creatorNames":[{"creatorName":"廣瀬, 孝","creatorNameLang":"ja"},{"creatorName":"Hirose, Takashi","creatorNameLang":"en"}]},{"creatorNames":[{"creatorName":"Matsukura, Yukinori","creatorNameLang":"en"},{"creatorName":"松倉, 公憲","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"Aoki, Hisashi","creatorNameLang":"en"},{"creatorName":"青木, 久","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"Kangawa, Takuma","creatorNameLang":"en"},{"creatorName":"寒川, 拓磨","creatorNameLang":"ja"}]},{"creatorNames":[{"creatorName":"前門, 晃","creatorNameLang":"ja"},{"creatorName":"Maekado, Akira","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_1617186609386":{"attribute_name":"Subject","attribute_value_mlt":[{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"円錐カルスト"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"第四紀琉球石灰岩"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"斜面勾配"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"沖縄島"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"宮古島"},{"subitem_1522299896455":"ja","subitem_1522300014469":"Other","subitem_1523261968819":"Cone karst"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Quaternary Ryukyu Limestone"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"slope angle"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Okinawa Island"},{"subitem_1522299896455":"en","subitem_1522300014469":"Other","subitem_1523261968819":"Miyako Island"}]},"item_1617186626617":{"attribute_name":"Description","attribute_value_mlt":[{"subitem_description":"本研究では，第四紀琉球石灰岩地域に発達する円錐カルストに着目し，現地写真測量により，その形態の調査を行い，従来から円錐カルストの発達が知られている本部山里の円錐カルストの形態との比較を行った．その結果，中古生代の石灰岩地域である沖縄島本部山里に発達する円錐カルストに比較して，第四紀琉球石灰岩地域の円錐カルストは，斜面勾配が小さく，頂点標高も低いという特徴がみられた．","subitem_description_language":"ja","subitem_description_type":"Other"}]},"item_1617186643794":{"attribute_name":"Publisher","attribute_value_mlt":[{"subitem_1522300295150":"ja","subitem_1522300316516":"沖縄地理学会"},{"subitem_1522300295150":"en","subitem_1522300316516":"The Okinawa Geographical Society"}]},"item_1617186702042":{"attribute_name":"Language","attribute_value_mlt":[{"subitem_1551255818386":"jpn"}]},"item_1617186920753":{"attribute_name":"Source 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