{"@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/1363670320622994816.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/1998tc900011"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F1998TC900011"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1998TC900011"}},{"identifier":{"@type":"NAID","@value":"30013375817"}}],"dc:title":[{"@value":"Trench‐parallel stretching and folding of forearc basins and lateral migration of the accretionary wedge in the southern Ryukyus: A case of strain partition caused by oblique convergence"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Detailed seafloor mapping in the area east of Taiwan revealed trench‐parallel stretching and folding of the Ryukyu forearc and lateral motion of the accretionary wedge under oblique convergence. East of 122°40′E, a steep accretionary wedge is elongated in an E–W direction. A major transcurrent right‐lateral strike‐slip fault accommodates the strain partitioning caused by an oblique convergence of 40°. A spectacular out‐of‐sequence thrust may be related to the subduction of a structural high lying in the axis of the N–S trending Gagua Ridge. This asperity is likely responsible for the uplift of the accretionary wedge and forearc basement and may have augmented strain partitioning by increasing the coupling between the two plates. West of 122°40′E, the low‐taper accretionary wedge is sheared in a direction subparallel to the convergence vector with respect to the Ryukyu Arc. The bayonet shape of the southern Ryukyu Arc slope partly results from the recent (re)opening of the southern Okinawa Trough at a rate of about 2 to 4 cm/yr. Right‐lateral shearing of the sedimentary forearc with respect to the nonlinear Ryukyu backstop generates trench‐parallel extension in the forearc sediment sequence at dilational jogs and trench‐parallel folding at compressive jogs. The Hoping Basin lies above a diffuse trench/trench/fault (TTF) or TFF unstable triple junction moving toward the south along a N–S transform zone which accommodates the southward drift of the Ryukyu Arc with respect to Eurasia.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383670320622994817","@type":"Researcher","foaf:name":[{"@value":"Serge Lallemand"}]},{"@id":"https://cir.nii.ac.jp/crid/1380579817433530752","@type":"Researcher","foaf:name":[{"@value":"Char‐Shine Liu"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320622994818","@type":"Researcher","foaf:name":[{"@value":"Stéphane Dominguez"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320622994816","@type":"Researcher","foaf:name":[{"@value":"Philippe Schnürle"}]},{"@id":"https://cir.nii.ac.jp/crid/1383670320622994820","@type":"Researcher","foaf:name":[{"@value":"Jacques Malavieille"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"02787407"},{"@type":"EISSN","@value":"19449194"},{"@type":"NCID","@value":"AA10628803"}],"prism:publicationName":[{"@value":"Tectonics"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1999-04","prism:volume":"18","prism:number":"2","prism:startingPage":"231","prism:endingPage":"247"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F1998TC900011"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/1998TC900011"}],"createdAt":"2002-09-17","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360567183441972992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Accretionary prism collapse: a new hypothesis on the source of the 1771 giant tsunami in the Ryukyu Arc, SW Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360584340699222144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deformation microstructures of low- and high-strain epidote-blueschist (Ryukyu arc, Japan): Implications for subduction interface rheology"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204229438208","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Tectonic and Paleoseismological Significance of Holocene Marine Terraces on the East Coast of Coastal Range, Taiwan."},{"@value":"台湾海岸山脈東岸の完新世海成段丘と地殻変動"},{"@language":"ja-Kana","@value":"タイワン カイガン サンミャク トウガン ノ カンシン セイ カイセイ ダンキュウ ト チカク ヘンドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681217169792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Submarine slides and marine geohazards:"},{"@language":"ja","@value":"海底地すべりと災害"},{"@value":"海底地すべりと災害 : これまでの研究成果と現状の問題点"},{"@language":"ja-Kana","@value":"カイテイ ジスベリ ト サイガイ : コレマデ ノ ケンキュウ セイカ ト ゲンジョウ ノ モンダイテン"},{"@value":"Submarine slides and marine geohazards: the study results so far and current problems"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433316893073024","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Distribution of low-frequency earthquakes accompanying the very low frequency earthquakes along the Ryukyu Trench"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/1998tc900011"},{"@type":"CIA","@value":"30013375817"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2017.0031_references_DOI_WjiefEoMXe3swMrNB38wE1rwhns"},{"@type":"CROSSREF","@value":"10.1186/s40623-017-0632-4_references_DOI_WjiefEoMXe3swMrNB38wE1rwhns"},{"@type":"CROSSREF","@value":"10.1038/s41598-018-31956-8_references_DOI_WjiefEoMXe3swMrNB38wE1rwhns"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2023.105041_references_DOI_WjiefEoMXe3swMrNB38wE1rwhns"}]}