{"@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/1361699994816466304.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/0040-1951(93)90036-j"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:004019519390036J?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:004019519390036J?httpAccept=text/plain"}},{"identifier":{"@type":"NAID","@value":"30004173955"}}],"dc:title":[{"@value":"The evidence of along-arc differential uplift of the Shimanto accretionary complex: Fission track thermochronology of the Kumano Acidic Rocks, Southwest Japan"}],"description":[{"notation":[{"@value":"Abstract   The Kumano Acidic Rocks (KARs) are the most extensive of the Tertiary granitic bodies in the southwest Japanese fore-arc. They intrude the Cretaceous-lower Miocene Shimanto accretionary complex, perturbing its initial thermal records related to accretion. To assess the timing of igneous activity and subsequent cooling history of the KARs, fission-track (FT) ages were measured on seventeen zircon and three apatite samples, along with four zircon confined track-lengths. Samples were collected mainly from the Granite Porphyry of the KARs along two traverses intersecting expected isotherms. Zircon and apatite ages show good agreement at approximately 15 Ma and, in conjunction with the observed track-lengths, suggest rapid uniform cooling of the KARs in the temperature range ~ 100− ~ 300°C. In addition, based on the petrographie features of the KARs, the inferred thermal history is best explained by rapid cooling subsequent to the eruption of felsic magma. The rapid cooling of the KARs at approximately 15 Ma indicates that the basement Shimanto accretionary complex in the area had already cooled at that time. FT apatite ages of ~ 10 Ma were reported in the Muroto Peninsula, which is about 100 km southwest of the Kii Peninsula. These contrasting results suggest differential uplift of the Shimanto accretionary complex along its length, presumably caused by some features characterizing the subducting Shikoku Basin. Furthermore, the cooling age of the KARs places constraints on the ages of the  Orbulina  Datum and the clockwise rotation of Southwest Japan."}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699994816466305","@type":"Researcher","foaf:name":[{"@value":"Noriko Hasebe"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994816466306","@type":"Researcher","foaf:name":[{"@value":"Takahiro Tagami"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699994816466304","@type":"Researcher","foaf:name":[{"@value":"Susumu Nishimura"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"1993-09","prism:volume":"224","prism:number":"4","prism:startingPage":"327","prism:endingPage":"335"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:004019519390036J?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:004019519390036J?httpAccept=text/plain"}],"createdAt":"2003-08-07","modifiedAt":"2019-03-15","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360285710504477056","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Paleomagnetic constraints on <scp>M</scp>iocene rotation in the central <scp>J</scp>apan <scp>A</scp>rc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185481194880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Instantaneous paleomagnetic record from the <scp>M</scp>iocene <scp>K</scp>ozagawa <scp>D</scp>ike of the <scp>K</scp>umano <scp>A</scp>cidic <scp>R</scp>ocks, <scp>K</scp>ii <scp>P</scp>eninsula, <scp>S</scp>outhwest <scp>J</scp>apan: cautionary note on tectonic interpretation"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861295472451328","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extensional stress accompanied by Miocene near-trench magmatism in the southern Kii Peninsula, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360865815502197376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Thermochronology of hydrothermal alteration zones in the Kii Peninsula, southwest Japan: an attempt for detecting the thermal anomalies and implications to the regional exhumation history"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206234285568","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Multiple tectonic events in the Miocene Japan arc: The Heike microplate hypothesis."},{"@language":"ja","@value":"日本列島周辺の中新世プレート運動: 平家プレート仮説"},{"@value":"Multiple tectonic events in the Miocene Japan arc: the Heike microplate hypothesis. Journal of Mineralogy"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237453184","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Temporal relationship between the northern and the southern parts of the Kumano Acidic Rocks and the Muro Pyroclastic Flow Deposit, Kii Peninsula, Japan, examined by comparison of paleomagnetic directions"},{"@language":"ja","@value":"古地磁気方位の比較からみた熊野酸性岩類北部と南部及び室生火砕流堆積物の時間関係"},{"@language":"ja-Kana","@value":"コ チジキ ホウイ ノ ヒカク カラ ミタ クマノ サンセイガンルイ ホクブ ト ナンブ オヨビ ムロウ カサイリュウ タイセキブツ ノ ジカン カンケイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237546752","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fission track ages on apatite from Miocene igneous rocks in the Kii Peninsula, Japan"},{"@language":"ja","@value":"紀伊半島，中新世火成岩類のアパタイトのフィッション・トラック年代"},{"@language":"ja-Kana","@value":"キイハントウ チュウシンセイ カセイガンルイ ノ アパタイト ノ フィッション トラック ネンダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238160128","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleomagnetism and rock magnetism of Miocene dikes in the Nakaoku area, Nara Prefecture, central Kii Peninsula, Japan"},{"@language":"ja","@value":"紀伊半島中央部, 奈良県中奥地域にみられる中新世岩脈の古地磁気と岩石磁気"},{"@language":"ja-Kana","@value":"キイハントウ チュウオウブ ナラケン ナカ オクチイキ ニ ミラレル チュウシンセイガン ミャク ノ コ チジキ ト ガンセキ ジキ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238395648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Vertical structure and emplacement process of the North Unit of the Middle Miocene Kumano Acidic Rocks, Southwest Japan, inferred from the GSJ Kumano-Ichiura drill core"},{"@language":"ja","@value":"熊野井内浦掘削コアから推測する中期中新世熊野酸性岩北岩体の垂直構造と定置過程"},{"@language":"ja-Kana","@value":"クマノ イチウラ クッサク コア カラ スイソク スル チュウキ チュウシンセイ クマノ サンセイガン ホクガンタイ ノ スイチョク コウゾウ ト テイチ カテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206544986368","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Paleomagnetism of the Nijo Group and its implication for the timing of clockwise rotation of southwest Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1390001288101144704","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonics of sedimentary basins in and around Japan since the opening of the Sea of Japan"},{"@language":"ja","@value":"日本海拡大以来の日本列島の堆積盆テクトニクス"},{"@language":"ja-Kana","@value":"ニホンカイ カクダイ イライ ノ ニホン レットウ ノ タイセキボン テクトニクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282680171720064","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"熊野酸性火成岩類の古地磁気方位"},{"@language":"en","@value":"Paleomagnetic direction of the Kumano Acidic Igneous Rocks, Kii peninsula, Japan."},{"@language":"ja-Kana","@value":"クマノ サンセイ カセイガンルイ ノ コ チジキ ホウイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681211559808","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fission-track dating of the Shionomisaki Igneous Complex, Kii Peninsula, Japan."},{"@value":"紀伊半島，潮岬火成複合岩類のフィッション・トラック年代測定"},{"@language":"ja-Kana","@value":"キイハントウ シオノミサキ カセイフクゴウガンルイ ノ フイッション トラック ネンダイ ソクテイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213561984","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Simultaneity and similarity of the Muro Pyroclastic Flow Deposit and the Kumano Acidic Rocks in Kii Peninsula, southwest Japan, based on fission track ages and morphological characteristics of zircon"},{"@language":"ja","@value":"ジルコンのフィッション・トラック年代と特徴からみた室生火砕流堆積物と熊野酸性岩類の同時性と類似性"},{"@language":"ja-Kana","@value":"ジルコン ノ フィッション トラック ネンダイ ト トクチョウ カラ ミタ ムロウ カサイリュウ タイセキブツ ト クマノ サンセイガンルイ ノ ドウジセイ ト ルイジセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213564032","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Widespread correlation of Middle Miocene tephras in Japan: a possible link between the Kn-1 tuff (Boso Peninsula) and the Muro Pyroclastic Flow Deposit (Kii Peninsula)"},{"@language":"ja","@value":"中期中新世テフラの広域対比：房総半島Kn-1凝灰岩と紀伊半島室生火砕流堆積物"},{"@language":"ja-Kana","@value":"チュウキ チュウシンセイ テフラ ノ コウイキ タイヒ ボウソウ ハントウ Kn 1 ギョウカイガン ト キイ ハントウ ムロウ カサイリュウ タイセキブツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213584768","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A ring dike and a subhorizontal sheet intrusion in a volcano-plutonic complex: geology of the Kumano Acidic Rocks in the Owase-Kumano area, Kii Peninsula, Japan"},{"@language":"ja","@value":"火山－深成複合岩体にみられる環状岩脈とシート状貫入岩：紀伊半島，尾鷲－熊野地域の熊野酸性火成岩類の地質"},{"@language":"ja-Kana","@value":"カザン シンセイ フクゴウガンタイ ニ ミラレル カンジョウ ガンミャク ト シートジョウ カンニュウガン キイ ハントウ オワセ クマノ チイキ ノ クマノ サンセイ カセイガンルイ ノ チシツ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390293969064573824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Zircon U-Pb and fission-track ages of felsic tuff from the Ryujin Complex in the Shimanto Accretionary Prism on the eastern part of the Kii Peninsula, Japan"},{"@language":"ja","@value":"紀伊半島東部の四万十付加体竜神コンプレックスに挟在する珪長質凝灰岩のジルコンU-Pb及びフィッション・トラック年代"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845713030086912","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Miocene clockwise rotation of Southwest Japan"},{"@language":"ja","@value":"中新世における西南日本の時計回り回転"},{"@language":"ja-Kana","@value":"チュウシンセイ ニ オケル セイナン ニホン ノ トケイ マワリ 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