{"@context":{"@vocab":"https://cir.nii.ac.jp/schema/1.0/","rdfs":"http://www.w3.org/2000/01/rdf-schema#","dc":"http://purl.org/dc/elements/1.1/","dcterms":"http://purl.org/dc/terms/","foaf":"http://xmlns.com/foaf/0.1/","prism":"http://prismstandard.org/namespaces/basic/2.0/","cinii":"http://ci.nii.ac.jp/ns/1.0/","datacite":"https://schema.datacite.org/meta/kernel-4/","ndl":"http://ndl.go.jp/dcndl/terms/","jpcoar":"https://github.com/JPCOAR/schema/blob/master/2.0/"},"@id":"https://cir.nii.ac.jp/crid/1390282679209540480.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.15080/agcjchikyukagaku.43.1_1"}},{"identifier":{"@type":"NDL_BIB_ID","@value":"3216983"}},{"identifier":{"@type":"URI","@value":"http://id.ndl.go.jp/bib/3216983"}},{"identifier":{"@type":"URI","@value":"https://ndlsearch.ndl.go.jp/books/R000000004-I3216983"}},{"identifier":{"@type":"NAID","@value":"110007092101"}}],"dc:title":[{"@language":"ja","@value":"琉球列島,伊平屋島・野甫島の完新世後期海水準変動"},{"@language":"en","@value":"Late Holocene sea-level changes in Iheya and Noho Islands, the Ryukyus, Japan"},{"@value":"琉球列島,伊平屋島・野甫島の完新世後期海水準変動〔英文〕"},{"@language":"ja-Kana","@value":"リュウキュウ レットウ イヘヤジマ ノ"}],"dc:language":"en","description":[{"type":"abstract","notation":[{"@language":"en","@value":"Several indicators of a slightly higher Holocene sea level, reaching about 2 m above the present situation, have been found along the coasts of Iheya and Noho Islands. They include corals in a growth position, notches, beachrocks and an emerged coral reef distributed continuously along the northernmost coastal stretch of Iheya Island. Several radiocarbon datings have provided ages between 4,650 and 1,580 yr BP. No evidence of abrupt uplifts datings from Holocene time could be observed."},{"@language":"ja","@value":"現海面上約2メートルまでの完新世高位海水準を,琉球列島の伊平屋島およびその南の野甫島で認めた.旧汀線指示物として厚地性サンゴ,ノッチ,ビーチロック,そして離水サンゴ礁面を使用した.離水サンゴ礁面は伊平屋島北端の海岸に連続して分布する.これらの旧汀線指示物の8試料について^<14>C年代測定を行い,4,650年前から1,580年前の年代を得た.完新世後期において,地良性地殻変動に基づく急激な海水準の変動は認められなかった."}],"abstractLicenseFlag":"disallow"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1410001204267210369","@type":"Researcher","personIdentifier":[{"@type":"NRID","@value":"9000006912372"}],"foaf:name":[{"@language":"ja","@value":"ピラツォリ P. A."},{"@language":"en","@value":"Pirazzoli Paolo A."}],"jpcoar:affiliationName":[{"@language":"en","@value":"CNRS-Intergeo"}]},{"@id":"https://cir.nii.ac.jp/crid/1030003658311140995","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40141949"},{"@type":"NRID","@value":"1000040141949"},{"@type":"CINII_AUTHOR_ID","@value":"DA06707864"},{"@type":"URI","@value":"https://ci.nii.ac.jp/author/DA06707864#entity"},{"@type":"URI","@value":"https://viaf.org/viaf/NII%7CDA06707864"},{"@type":"NRID","@value":"9000023610783"},{"@type":"NRID","@value":"9000023610884"},{"@type":"NRID","@value":"9000023610805"},{"@type":"NRID","@value":"9000023619073"},{"@type":"NRID","@value":"9000023603621"},{"@type":"NRID","@value":"9000023624693"},{"@type":"NRID","@value":"9000302394583"},{"@type":"NRID","@value":"9000023640285"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0049143"}],"foaf:name":[{"@language":"ja","@value":"木庭 元晴"},{"@language":"en","@value":"Koba Motoharu"}],"jpcoar:affiliationName":[{"@language":"en","@value":"Institute of Geography, Faculty of Letters, Kansai University"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"03666611"},{"@type":"EISSN","@value":"21897212"},{"@type":"NDL_BIB_ID","@value":"000000014627"},{"@type":"ISSN","@value":"03666611"},{"@type":"LISSN","@value":"03666611"},{"@type":"NCID","@value":"AN00141269"}],"prism:publicationName":[{"@language":"ja","@value":"地球科学"},{"@language":"en","@value":"Earth Science (Chikyu Kagaku)"},{"@language":"ja","@value":"地球科学"},{"@language":"en","@value":"Chikyu Kagaku"},{"@language":"ja","@value":"地球科學"}],"dc:publisher":[{"@language":"en","@value":"The Association for the Geological Collaboration in Japan"},{"@language":"ja","@value":"地学団体研究会"}],"prism:publicationDate":"1989","prism:volume":"43","prism:number":"1","prism:startingPage":"1","prism:endingPage":"6"},"url":[{"@id":"http://id.ndl.go.jp/bib/3216983"},{"@id":"https://ndlsearch.ndl.go.jp/books/R000000004-I3216983"}],"availableAt":"1989","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1390282679206696704","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@value":"沖縄トラフの拡大運動からみた琉球列島中北部の完新世傾動運動"},{"@language":"en","@value":"Holocene Tilting in the Northern and Central Ryukyu Islands, as Deduced from Expansion of the Okinawa Trough"},{"@language":"ja-Kana","@value":"オキナワ トラフ ノ カクダイ ウンドウ カラ ミタ リュウキュウ レットウ チュウホクブ ノ カンシン セイケイドウ ウンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367078667776","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Submarine terraces reveal Late Quaternary tectonic deformation in the intermediate zone between the island shelf and rift zone of the middle part of the Nanseishoto Islands, southwest Japan"}]}],"dataSourceIdentifier":[{"@type":"JALC","@value":"oai:japanlinkcenter.org:2002484625"},{"@type":"NDL_SEARCH","@value":"oai:ndlsearch.ndl.go.jp:R000000004-I3216983"},{"@type":"CIA","@value":"110007092101"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01395-3_references_DOI_LCPgJ9ePh1efzSDxyhUS2g0mmIA"}]}