{"@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/1360855569100965632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1111/j.1440-1738.1998.00193.x"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1998.00193.x"}},{"identifier":{"@type":"URI","@value":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1998.00193.x"}}],"dc:title":[{"@value":"Arc–arc collision in the Izu collision zone, central Japan, deduced from the Ashigara Basin and adjacent Tanzawa Mountains"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The Pleistocene Ashigara Basin and adjacent Tanzawa Mountains, Izu collision zone, central Japan, are examined to better understand the development of an arc–arc orogeny, where the Izu–Bonin – Mariana (IBM) arc collides with the Honshu Arc. Three tectonic phases were identified based on the geohistory of the Ashigara Basin and the denudation history of the Tanzawa Mountains. In phase I, the IBM arc collided with the Honshu Arc along the Kannawa Fault. The Ashigara Basin formed as a trench basin, filled mainly by thin‐bedded turbidites derived from the Tanzawa Mountains together with pyroclastics. The Ashigara Basin subsided at a rate of 1.7 mm/year, and the denudation rate of the Tanzawa Mountains was 1.1 mm/year. The onset of Ashigara Basin Formation is likely to be older than 2.2 Ma, interpreted as the onset of collision along the Kannawa Fault. Significant tectonic disruption due to the arc–arc collision took place in phase II, ranging from 1.1 to 0.7 Ma in age. The Ashigara Basin subsided abruptly (4.6 mm/year) and the accumulation rate increased to approximately 10 times that of phase I. Simultaneously, the Tanzawa Mountains were abruptly uplifted. A tremendous volume of coarse‐grained detritus was provided from the Tanzawa Mountains and deposited in the Ashigara Basin as a slope‐type fan delta. In phase III, 0.7–0.5 Ma, the entire Ashigara Basin was uplifted at a rate of 3.6 mm/year. This uplift was most likely caused by isostatic rebound resulting from stacking of IBM arc crust along the Kannawa Fault which is not active as the decollement fault by this time. The evolution of the Ashigara Basin and adjacent Tanzawa Mountains shows a series of the development of the arc–arc collision; from the subduction of the IBM arc beneath the Honshu Arc to the accretion of IBM arc crust onto Honshu. Arc–arc collision is not the collision between the hard crusts (massif) like a continent–continent collision, but crustal stacking of the subducting IBM arc beneath the Honshu Arc intercalated with very thick trench fill deposits.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380855569100965504","@type":"Researcher","foaf:name":[{"@value":"WONN SOH"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569100965505","@type":"Researcher","foaf:name":[{"@value":"KAZUO NAKAYAMA"}]},{"@id":"https://cir.nii.ac.jp/crid/1380855569100965632","@type":"Researcher","foaf:name":[{"@value":"TAKU KIMURA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"10384871"},{"@type":"EISSN","@value":"14401738"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/10384871"}],"prism:publicationName":[{"@value":"Island Arc"}],"dc:publisher":[{"@value":"Wiley"}],"prism:publicationDate":"1998-07","prism:volume":"7","prism:number":"3","prism:startingPage":"330","prism:endingPage":"341"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1111%2Fj.1440-1738.1998.00193.x"},{"@id":"https://onlinelibrary.wiley.com/doi/pdf/10.1111/j.1440-1738.1998.00193.x"}],"createdAt":"2004-09-29","modifiedAt":"2023-10-28","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360283691038658176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transformation of juvenile Izu–Bonin–Mariana oceanic arc into mature continental crust: An example from the Neogene Izu collision zone granitoid plutons, Central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285707500168192","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Simulation of tectonic evolution of the Kanto Basin of Japan since 1 Ma due to subduction of the Pacific and Philippine Sea plates and the collision of the Izu-Bonin arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165262633088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Petrogenesis of the Kaikomagatake granitoid pluton in the Izu Collision Zone, central Japan: implications for transformation of juvenile oceanic arc into mature continental crust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179756104704","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A magma‐hydrothermal system beneath Hakone volcano, central Japan, revealed by highly resolved velocity structures"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567186205261440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Izu–Bonin Arc"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848660458000896","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Migration of a volcanic front inferred from <scp>K</scp>–<scp>A</scp>r ages of late <scp>M</scp>iocene to <scp>P</scp>liocene volcanic rocks in central <scp>J</scp>apan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360857593678663040","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Low-temperature thermochronology of active arc-arc collision zone, South Fossa Magna region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418518486045824","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Magma Reservoir and Magmatic Feeding System Beneath Hakone Volcano, Central Japan, Revealed by Highly Resolved Velocity Structure"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206237705984","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Distribution of tonalitic soil structure and geochemistry in the western part of Tanzawa Mountains: Construction of basic data for long-term monitoring study"},{"@language":"ja","@value":"西丹沢中川上流域に分布するトーナル岩母材土壌の構造と地球化学的特性：長期モニタリングに向けた基盤データの構築"},{"@language":"ja-Kana","@value":"ニシタンザワ ナカガワ ジョウリュウイキ ニ ブンプスル トーナルガン ボザイ ドジョウ ノ コウゾウ ト チキュウ カガクテキ トクセイ チョウキ モニタリング ニ ムケタ キバン データ ノ コウチク"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206238700032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"An attempt on the estimation of permeability at depth in laboratory tests : A case of the Ashigara Group"},{"@language":"ja","@value":"室内実験による地下深部の浸透率構造の推定－足柄層群を例として－"},{"@language":"ja-Kana","@value":"シツナイ ジッケン ニ ヨル チカ シンブ ノ シントウリツ コウゾウ ノ スイテイ アシガラソウグン オ レイ ト シテ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206525953536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"K-Ar ages of volcanic rocks in the Tanzawa-Oiso area, central Japan: Implication for westward migration of the Pliocene volcanic front in the southern Fossa Magna region"},{"@language":"ja","@value":"丹沢-大磯地域に分布する火山岩類の K-Ar 年代と南部フォッサマグナ地域における鮮新世火山フロントの西方移動"},{"@language":"ja-Kana","@value":"タンザワ-オオイソ チイキ ニ ブンプ スル カザンガンルイ ノ K-Ar ネンダイ ト ナンブ フォッサマグナ チイキ ニ オケル センシンセイ カザン フロント ノ サイホウ イドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679529390208","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Hydrochemistry of the groundwaters in the Izu collision zone and its adjacent eastern area, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213889280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Overview of scientific results of the deep drilling project of the Chelungpu Fault, upon which the 1999 Chi-Chi (Taiwan) earthquake occurred: Main findings and future research"},{"@language":"ja","@value":"1999年台湾集集地震を引き起こしたチェルンプ断層の深部掘削の成果概要－明らかになってきた断層岩の物質科学と今後の課題－"},{"@language":"ja-Kana","@value":"1999ネン タイワンシュウシュウ ジシン オ ヒキオコシタ チェルンプ ダンソウ ノ シンブ クッサク ノ セイカ ガイヨウ アキラカ ニ ナッテ キタ ダンソウガン ノ ブッシツ カガク ト コンゴ ノ カダイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218251136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geology of the Tanzawa Mountains, Japan:"},{"@language":"ja","@value":"丹沢山地の地質："},{"@value":"丹沢山地の地質 : 伊豆衝突帯のジオダイナミクス"},{"@language":"ja-Kana","@value":"タンザワ サンチ ノ チシツ : イズ ショウトツタイ ノ ジオダイナミクス"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681218890112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geological structure of the Izu collision zone, northern border of the Izu block, southern Kanto, Japan"},{"@language":"ja","@value":"伊豆地塊北端部，伊豆衝突帯の地質構造"}]},{"@id":"https://cir.nii.ac.jp/crid/1390566775145816320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of emplacement depth for the Miocene Kaikomagatake granitoid pluton: constraints on crustal denudation history of the Izu collision zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390860542683886464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A Review of Recent Research on Crustal Structures and Seismo-tectonics of the Izu Collision Zone"},{"@language":"ja","@value":"伊豆衝突帯とその周辺における地殻構造と地震テクトニクス"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892078330752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Isolated intermediate-depth seismicity north of the Izu peninsula, Japan : implications for subduction of the Philippine Sea Plate"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1111/j.1440-1738.1998.00193.x"},{"@type":"OPENAIRE","@value":"doi_dedup___::8673e99ae825de75995d38bd207f742c"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0779-7_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1016/j.lithos.2016.07.035_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.5575/geosoc.113.27_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.5575/geosoc.113.611_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.5575/geosoc.115.488_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.4294/zisin.2023-9s_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1007/s00410-011-0689-1_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1002/2014jb011856_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1144/goj.7_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.2465/gkk.111024_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2016.0030_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.5575/geosoc.117.s135_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1111/iar.12073_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2016.04.005_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.2343/geochemj.1.0124_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2022.229231_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.1029/2020jb021236_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"},{"@type":"CROSSREF","@value":"10.2465/jmps.191031_references_DOI_X9ZjAveNgTM5dt6mpssSRcIkS11"}]}