{"@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/1364233270723929344.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/jb091ib12p12661"}},{"identifier":{"@type":"URI","@value":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB091iB12p12661"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB091iB12p12661"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB091iB12p12661"}},{"identifier":{"@type":"NAID","@value":"30034752945"}}],"dc:title":[{"@value":"Dislocation model for aseismic crustal deformation at Hollister, California"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Geodetic observations at many active plate margins reveal relatively steady aseismic motion during the time between major earthquakes. We model the aseismic motion by the relative motion between several blocks that suffer frictional resistance in the upper crust. Frictional drag is represented by uniform dislocation on a fault surface. We assume that friction occurs only on the upper “brittle zone” of each block boundary and that frictionless sliding occurs below this zone. Using a Bayesian inversion procedure, we invert geodetic data to determine the parameters of the block and dislocation model. Parameters to be estimated include the two horizontal components of velocity for each block and the dislocation rate, dip angle, slip angle, and width of each rectangular fault patch. For Hollister we assume five blocks and nine rectangular fault patches. Rates of length change on 92 lines observed by trilateration make up the data. Triangulation, leveling, very long baseline interferometry, satellite ranging, and global positioning system data can also be easily included in our model. Our inversion procedure uses prior estimates of all block and fault parameters based on geological and seismological data. The block parameters are estimated from geological observations of fault displacement rates, while the widths of the fault patches are estimated from earthquake hypocentral depths. We choose prior estimates of the dislocation rate to match observed creep rates. The estimated block motion is well resolved by the geodetic data and agrees well with the geological estimates. This suggests that the block motion is steady on time scales from 10 years to 1 m.y. The net motion across the San Andreas‐Calaveras fault system is 38 ± 3 mm/yr oriented S38°E. Thus some additional displacement, possibly offshore, is needed to match the rate of 56 mm/yr predicted by plate tectonic models. The depth of the transition from frictional to free sliding varies considerably, from 0.4 km on the southern Calaveras to 11 km on the central San Andreas fault. Two segments of the San Andreas, north of 36°50′ and south of 36°40′, have the greatest potential for moderate to large earthquakes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1384233270723929344","@type":"Researcher","foaf:name":[{"@value":"Mitsuhiro Matsu'ura"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270723929345","@type":"Researcher","foaf:name":[{"@value":"David D. Jackson"}]},{"@id":"https://cir.nii.ac.jp/crid/1384233270723929346","@type":"Researcher","foaf:name":[{"@value":"Abe Cheng"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1986-11-10","prism:volume":"91","prism:number":"B12","prism:startingPage":"12661","prism:endingPage":"12674"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"http://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB091iB12p12661"},{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2FJB091iB12p12661"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/JB091iB12p12661"}],"createdAt":"2008-02-06","modifiedAt":"2023-09-23","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050866882758946304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Geodetic data inversion to estimate a strain-rate field by introducing sparse modeling"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233290444800","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A small persistent locked area associated with the 2011 <i>M</i><sub>w</sub>9.0 Tohoku‐Oki earthquake, deduced from GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360025431099443584","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Numerical experiment toward simultaneous estimation of the spatiotemporal evolution of interseismic fault slips and block motions in southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710979665536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strain partitioning and interplate coupling along the northern margin of the Philippine Sea plate, estimated from Global Navigation Satellite System and Global Positioning System-Acoustic data"}]},{"@id":"https://cir.nii.ac.jp/crid/1360286994500115200","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Introduction of covariance components in slip inversion of geodetic data following a non-uniform spatial distribution and application to slip deficit rate estimation in the Nankai Trough subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306906098786816","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Second-order smoothness prior over the Delaunay Tessellation in Bayesian geophysical inversion"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567179755972352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geodetic imaging of potential seismogenic asperities on the Xianshuihe‐Anninghe‐Zemuhe fault system, southwest China, with a new 3‐D viscoelastic interseismic coupling model"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567184543044096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Interseismic GPS strain data inversion to estimate slip-deficit rates at plate interfaces: application to the Kanto region, central Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204067817856","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Elucidation of Interplate Coupling Based on Geodetic Data"},{"@language":"ja","@value":"測地学的データに基づくプレート間相互作用の解明"},{"@language":"ja-Kana","@value":"ソクチガクテキ データ ニ モトズク プレート カン ソウゴ サヨウ ノ カイメイ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204230243072","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Destructive Earthquake: Forecast and Disaster Prevention Measures. Strategy and Prospects for Earthquake Prediction."},{"@value":"地震災害を考える　　予測と対策　　地震予知の戦略と展望"},{"@language":"ja-Kana","@value":"ジシン ヨチ ノ センリャク ト テンボウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303055616","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The Process by Which Intraplate Earthquakes Are Generated"},{"@language":"ja","@value":"内陸地震の発生過程"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303129088","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of Study of Inversion Analyses Using ABIC in Seismology"},{"@language":"ja","@value":"地震学における ABIC を用いたインバージョン解析研究の進展"},{"@language":"ja-Kana","@value":"ジシンガク ニ オケル ABIC オ モチイタ インバージョン カイセキ ケンキュウ ノ シンテン"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204306509824","@type":"Article","relationType":["isCitedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"兵庫県南部地震の発生過程"},{"@language":"en","@value":"A Possible 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