{"@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/1360848657453500544.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1016/j.tecto.2013.07.022"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195113004630?httpAccept=text/xml"}},{"identifier":{"@type":"URI","@value":"https://api.elsevier.com/content/article/PII:S0040195113004630?httpAccept=text/plain"}}],"resourceType":"学術雑誌論文(journal article)","dc:title":[{"@value":"Temporal slip change based on curved slickenlines on fault scarps along Itozawa fault caused by 2011 Iwaki earthquake, northeast Japan"}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380848657453500549","@type":"Researcher","foaf:name":[{"@value":"Makoto Otsubo"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848657453500548","@type":"Researcher","foaf:name":[{"@value":"Norio Shigematsu"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848657453500544","@type":"Researcher","foaf:name":[{"@value":"Kazutoshi Imanishi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848657453500547","@type":"Researcher","foaf:name":[{"@value":"Ryosuke Ando"}]},{"@id":"https://cir.nii.ac.jp/crid/1420282801197341696","@type":"Researcher","personIdentifier":[{"@type":"KAKEN_RESEARCHERS","@value":"40470033"},{"@type":"NRID","@value":"1000040470033"},{"@type":"NRID","@value":"9000001998534"},{"@type":"NRID","@value":"9000004618940"},{"@type":"NRID","@value":"9000311498092"},{"@type":"NRID","@value":"9000399224099"},{"@type":"NRID","@value":"9000254263303"},{"@type":"NRID","@value":"9000267810247"},{"@type":"NRID","@value":"9000257916693"},{"@type":"NRID","@value":"9000346936623"},{"@type":"NRID","@value":"9000014233460"},{"@type":"RESEARCHMAP","@value":"https://researchmap.jp/read0138382"}],"foaf:name":[{"@value":"Miki Takahashi"}]},{"@id":"https://cir.nii.ac.jp/crid/1380848657453500545","@type":"Researcher","foaf:name":[{"@value":"Takashi Azuma"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00401951"},{"@type":"PISSN","@value":"http://id.crossref.org/issn/00401951"}],"prism:publicationName":[{"@value":"Tectonophysics"}],"dc:publisher":[{"@value":"Elsevier BV"}],"prism:publicationDate":"2013-11","prism:volume":"608","prism:startingPage":"970","prism:endingPage":"979"},"reviewed":"false","dc:rights":["https://www.elsevier.com/tdm/userlicense/1.0/"],"url":[{"@id":"https://api.elsevier.com/content/article/PII:S0040195113004630?httpAccept=text/xml"},{"@id":"https://api.elsevier.com/content/article/PII:S0040195113004630?httpAccept=text/plain"}],"createdAt":"2013-07-27","modifiedAt":"2023-07-03","project":[{"@id":"https://cir.nii.ac.jp/crid/1040282257242712960","@type":"Project","projectIdentifier":[{"@type":"KAKEN","@value":"25610150"},{"@type":"JGN","@value":"JP25610150"},{"@type":"URI","@value":"https://kaken.nii.ac.jp/grant/KAKENHI-PROJECT-25610150/"}],"notation":[{"@language":"ja","@value":"岩石の不安定挙動への分岐とその準備過程"},{"@language":"en","@value":"Bifurcation processes to shear-localization and unstable behavior of rock"}]}],"relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202065857280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The multiple inverse method: a new technique to separate stresses from heterogeneous fault-slip data"},{"@value":"The multiple inverse method: a new technique to separate stresses from heterogeneous fault-stop data"},{"@value":"Multiple inverse method: a new technique to separate stresses from heterogeneous fault-slip data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233288308864","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stress before and after the 2011 great Tohoku‐oki earthquake and induced earthquakes in inland areas of eastern Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360292620039256448","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Fault interaction may generate multiple slip vectors on a single fault surface"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298341430922752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic temporal changes of slip direction: The effect of absolute stress on dynamic rupture"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567188144044032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Simultaneous Reactivation of Two, Subparallel, Inland Normal Faults during the Mw 6.6 11 April 2011 Iwaki Earthquake Triggered by the Mw 9.0 Tohoku-oki, Japan, Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574094002846464","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"NIED seismic moment tensor catalogue for regional earthquakes around Japan: quality test and application"}]},{"@id":"https://cir.nii.ac.jp/crid/1360574096142604160","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surface Fault Ruptures and Slip Distributions of the Mw 6.6 11 April 2011 Hamadoori, Fukushima Prefecture, Northeast Japan, Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360576118818604800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic slickenlines record the emergence of multiple rupture fronts during a surface-breaking earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229814381696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic simulations of coseismic slickenlines on non-planar and rough faults"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663120748160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Complex Ruptures of the 11 April 2011 Mw 6.6 Iwaki Earthquake Triggered by the 11 March 2011 Mw 9.0 Tohoku Earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855570065756928","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"First‐ and second‐order patterns of stress in the lithosphere: The World Stress Map Project"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571244284032","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural Analysis of Coseismic Normal Fault Zones of the 2011 Mw 6.6 Fukushima Earthquake, Northeast Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360855571459639936","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural analysis and interpretation of the surface deformations of the El Asnam Earthquake of October 10, 1980"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861294957357056","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Use of fault striations and dislocation models to infer tectonic shear stress during the 1995 Hyogo-Ken Nanbu (Kobe) earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361137044845498752","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the inference of absolute stress levels from seismic radiation"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418519892898688","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Dynamic growth of mixed-mode shear cracks"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520085007360","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A stress inversion procedure for polyphase fault/slip data sets"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520671726080","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of the mean principal directions of stresses for a given fault population"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418520750308480","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Coseismic and postseismic slip of the 2011 magnitude-9 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1361418521476820992","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Surficial Slip and Rupture Geometry on the Beichuan Fault near Hongkou during the Mw 7.9 Wenchuan Earthquake, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981469343259520","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The 2011 Magnitude 9.0 Tohoku-Oki Earthquake: Mosaicking the Megathrust from Seconds to Centuries"}]},{"@id":"https://cir.nii.ac.jp/crid/1361981470496641920","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Structural analysis of the superficial deformation of the 1969 Pariahuanca earthquakes (Central Peru)"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943411986048","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"An inverse problem in microtectonics for the determination of stress tensors from fault striation analysis"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943593336320","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"The Mechanics of Oblique Slip Faulting"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262943836017792","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Computerized identification of stress tensors determined from heterogeneous fault-slip data by combining the multiple inverse method and k-means clustering"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262945527211648","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Stress, strain, and mountain building in central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1362262946288179968","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characterization of stress perturbations near major fault zones: insights from 2-D distinct-element numerical modelling and field studies (Jura mountains)"}]},{"@id":"https://cir.nii.ac.jp/crid/1363388844618300288","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geometry of Shearing Stress and Relation to Faulting"}]},{"@id":"https://cir.nii.ac.jp/crid/1363670321261110016","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Determination of stresses from heterogeneous focal mechanism data: An adaptation of the multiple inverse method"}]},{"@id":"https://cir.nii.ac.jp/crid/1363951795233402880","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Unusual shallow normal‐faulting earthquake sequence in compressional northeast Japan activated after the 2011 off the Pacific coast of Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1364233269026681344","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleostress analysis using the Hough transform for separating stresses from heterogeneous fault-slip data"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557257","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Original forms and initial modifications of the Galway Lake Road scarp formed along the Emerson fault during the 28 June 1992 Landers, California, earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557377","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Geological research on the Izu-Hanto-oki earthquake of 1974"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557380","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"On the curved striations of Nojima seismic fault engraved at the 1995 Hyogoken–Nanbu earthquake, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557381","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Analyse theorique et numerique d'un modele mecanique elementaire applique a l'e´tude d'une population de failes"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557385","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Paleostress inversion in a multiphase deformed area: kinematic and structural evolution of the Çankiri Basin (central Turkey), Part 1"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557389","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Tectonic setting of coseismic surface rupture associated with the 2011 Iwaki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557390","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Free software helps map and display data"}]},{"@id":"https://cir.nii.ac.jp/crid/1370006050269557392","@type":"Product","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"Characteristics of earthquake surface rupture along the Idosawa fault associated with the 2011 Fukushima Hamadori earthquake: normal faulting in trench-normal stretching forearc subsequent to the Tohoku mega-thrust earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303262336","@type":"Article","relationType":["references"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Rupture Process of the April 11, 2011 Fukushima Hamadori Earthquake (<I>M</I><SUB>j</SUB> 7.0)"},{"@language":"ja","@value":"2011年4月11日福島県浜通りの地震（<I>M</I><SUB>j</SUB>7.0）の震源過程"},{"@value":"Rupture Process of the April 11, 2011 Fukushima Hamadori Earthquake (Mj 7.0)"},{"@value":"Rupture process of the April 11, 2011 Fukushima Hamadori earthquake (Mj 7.0) —two fault planes inferred from strong motion and relocated aftershocks"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206241913472","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Uncertainty of faulting for long-term safety assessment in geological disposal"},{"@language":"ja","@value":"地層処分の長期安全を評価する際の断層活動における不確実性"},{"@language":"ja-Kana","@value":"チソウ ショブン ノ チョウキ アンゼン オ ヒョウカ スル サイ ノ ダンソウ カツドウ ニ オケル フカクジツセイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390021218874903808","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of kinematic history of the faults by fault geometry, composite planar fabric, and stress inversion analysis: Case study of the Yunodake Fault that was active during the 2011 Fukushima-ken Hamadori earthquake"},{"@language":"ja","@value":"断層幾何学，複合面構造，応力逆解析から推定した断層の運動像：2011年福島県浜通りの地震で活動した湯ノ岳断層の例"}]},{"@id":"https://cir.nii.ac.jp/crid/1390299837599444096","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Estimation of kinematic and stress history by composite planar fabric and stress inversion analysis: Application to the Shionohira and Kuruma faults"},{"@language":"ja","@value":"複合面構造と応力逆解析による断層の運動履歴および応力史の推定：塩ノ平断層と車断層への適用例"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942124916992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Normal-faulting stress state associated with low differential stress in an overriding plate in northeast Japan prior to the 2011 Mw 9.0 Tohoku earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792045164672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["references"],"jpcoar:relatedTitle":[{"@value":"A normal-faulting seismic sequence triggered by the 2011 off the Pacific coast of Tohoku Earthquake : wholesale stress regime changes in the upper plate"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1016/j.tecto.2013.07.022"},{"@type":"KAKEN","@value":"PRODUCT-15110069"},{"@type":"CROSSREF","@value":"10.1186/s40623-018-0813-9_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2021.228834_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"},{"@type":"CROSSREF","@value":"10.1093/gji/ggac501_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2024.0032_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2024.0001_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"},{"@type":"CROSSREF","@value":"10.5575/geosoc.2014.0042_references_DOI_QKly2t1CXmCWgKhK5x19CEEgTI4"}]}