{"@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/1361699993856718848.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/2004jb003541"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003541"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003541"}}],"dc:title":[{"@value":"Late Quaternary to decadal velocity fields in Asia"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>Fields of crustal velocity and strain rate within Asia, averaged over horizontal distances of ∼300 km, are calculated from estimates of Quaternary slip rates on faults and rates of change of lengths of baselines between GPS sites. The calculated fields fit strain rate components estimated from Quaternary slip rates within 95% confidence limits and fit the GPS data with an RMS residual of 2.5 mm yr<jats:sup>−1</jats:sup>. The strain rate field constrained only by Quaternary slip rates of faults differs from the combined solution at the level of 20 nstrain yr<jats:sup>−1</jats:sup>, and the differences are explicable by the limited accuracy of geological estimates of slip rate. Therefore the strain rate fields determined by geodetic measurements taken on the 10‐year timescale are consistent with geological observations on the 10<jats:sup>4</jats:sup>‐year timescale. The combined solution for velocities shows plate‐ or block‐like motion within deforming Asia only in Tarim, south China, and the Amurian region; elsewhere the kinematics of rigid blocks does not provide a useful description of the motion. In particular, velocities relative to Eurasia point at high angles to contours of their magnitudes, not parallel to them as they would if large regions moved as rigid blocks. The axes of principal horizontal compressional strain align with topographic gradients, in agreement with previous suggestions that Asia deforms as a continuum under the influence of gravity.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381699993856718720","@type":"Researcher","foaf:name":[{"@value":"Philip England"}],"jpcoar:affiliationName":[{"@value":"Department of Earth Sciences University of Oxford  Oxford UK"}]},{"@id":"https://cir.nii.ac.jp/crid/1381699993856718848","@type":"Researcher","foaf:name":[{"@value":"Peter Molnar"}],"jpcoar:affiliationName":[{"@value":"Department of Geological Sciences and Cooperative Institute for Research in Environmental Sciences University of Colorado  Boulder Colorado USA"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"2005-12","prism:volume":"110","prism:number":"B12","prism:startingPage":"B12401"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F2004JB003541"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/2004JB003541"}],"createdAt":"2005-12-06","modifiedAt":"2023-10-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050564285794446208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inelastic strain rate in the seismogenic layer of Kyushu Island, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1050867421579577216","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Inelastic strain in the hypocentral region of the 2000 Western Tottori earthquake (M 7.3) inferred from aftershock seismic moment tensors"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567185522934528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Present tectonics of the southeast of Russia as seen from GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848654735986944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Method for estimating the stress field from seismic moment tensor data based on the flow rule in plasticity theory"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204554360704","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Contribution of methane to total gas pressure in deep waters at lakes Nyos and Monoun (Cameroon, West Africa)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206513981312","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Present-day crustal motion in northeast China determined from GPS measurements"},{"@value":"Present-day crustal motion in northeast China determined from GPS measurement"}]},{"@id":"https://cir.nii.ac.jp/crid/1390294045393167872","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Strain-rate Field of Japan Estimated from GNSS Data and Its Interpretation Based on Inter- and Intra-arc Deformation"},{"@language":"ja","@value":"GNSSデータに基づく日本列島の歪み速度場と島弧間および島弧内変動"},{"@language":"ja-Kana","@value":"GNSS データ ニ モトズク ニホン レットウ ノ ヒズミ ソクドジョウ ト トウコ カン オヨビ トウコ ナイ ヘンドウ"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/2004jb003541"},{"@type":"CROSSREF","@value":"10.5026/jgeography.131.479_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0584-0_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.1186/bf03352642_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.1111/j.1365-246x.2010.04871.x_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01186-2_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.1002/2016gl070129_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"},{"@type":"CROSSREF","@value":"10.2343/geochemj.2.0250_references_DOI_BX4bskZdORWPb2mKisqdoKZtjF3"}]}