{"@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/1362262945492853632.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1084531"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1084531"}}],"dc:title":[{"@value":"Using 1-Hz GPS Data to Measure Deformations Caused by the Denali Fault Earthquake"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>The 3 November 2002 moment magnitude 7.9 Denali fault earthquake generated large, permanent surface displacements in Alaska and large-amplitude surface waves throughout western North America. We find good agreement between strong ground-motion records integrated to displacement and 1-hertz Global Positioning System (GPS) position estimates collected ∼140 kilometers from the earthquake epicenter. One-hertz GPS receivers also detected seismic surface waves 750 to 3800 kilometers from the epicenter, whereas these waves saturated many of the seismicinstruments in the same region. High-frequency GPS increases the dynamic range and frequency bandwidth of ground-motion observations, providing another tool for studying earthquake processes.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262945492853632","@type":"Researcher","foaf:name":[{"@value":"Kristine M. Larson"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences, University of Colorado, Boulder, CO 80309–0429, USA."},{"@value":"Center for Earthquake Research and Information, University of Memphis, Memphis, TN 38152, USA."},{"@value":"U.S. Geological Survey, Memphis, TN 38152, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945492853633","@type":"Researcher","foaf:name":[{"@value":"Paul Bodin"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences, University of Colorado, Boulder, CO 80309–0429, USA."},{"@value":"Center for Earthquake Research and Information, University of Memphis, Memphis, TN 38152, USA."},{"@value":"U.S. Geological Survey, Memphis, TN 38152, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262945492853634","@type":"Researcher","foaf:name":[{"@value":"Joan Gomberg"}],"jpcoar:affiliationName":[{"@value":"Department of Aerospace Engineering Sciences, University of Colorado, Boulder, CO 80309–0429, USA."},{"@value":"Center for Earthquake Research and Information, University of Memphis, Memphis, TN 38152, USA."},{"@value":"U.S. Geological Survey, Memphis, TN 38152, USA."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2003-05-30","prism:volume":"300","prism:number":"5624","prism:startingPage":"1421","prism:endingPage":"1424"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1084531"}],"createdAt":"2003-05-20","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050025031480691456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Observation of Earth's free oscillation by dense GPS array: After the 2011 Tohoku megathrust earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846641639189888","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Quasi real‐time fault model estimation for near‐field tsunami forecasting based on RTK‐GPS analysis: Application to the 2011 Tohoku‐Oki earthquake (<i>M</i><sub>w</sub> 9.0)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848662361216768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Sensing the earth crustal deformation with nano-strain resolution fiber-optic sensors"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303057664","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Recent Observation for Crustal Deformation on Land"},{"@language":"ja","@value":"陸域地殻変動観測の現状"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512706560","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Measuring ground deformations with 1-Hz GPS data: the 2003 Tokachi-oki earthquake (preliminary report)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488494720","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Large surface wave of the 2004 Sumatra-Andaman earthquake captured by the very long baseline kinematic analysis of 1-Hz GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488806528","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Source processes of the 2005West Off Fukuoka Prefecture earthquake and its largest aftershock inferred from strong motion and 1-Hz GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489147648","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A decade of GEONET: 1994-2003"},{"@value":"A decade of GEONET: 1994-2003--The continuous GPS observation in Japan and its impact on earthquake studies"},{"@language":"ja-Kana","@value":"decade of GEONET 1994 2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003 —The continuous GPS observation in Japan and its impact on earthquake studies—"},{"@value":"1994–2003 The continuous GPS observation in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observations in Japan and its impact on earthquake studies"},{"@value":"A decade of GEONET: 1994–2003—The continuous GPS observation in Japan and its impact on earthquake studies"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763022369664","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Role of Real-Time GNSS in Near-Field Tsunami Forecasting"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282763128053120","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Review on Near-Field Tsunami Forecasting from Offshore Tsunami Data and Onshore GNSS Data for Tsunami Early Warning"}]},{"@id":"https://cir.nii.ac.jp/crid/1390845712975788032","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Development of GNSS Buoy for a Synthetic Geohazard Monitoring System"}]},{"@id":"https://cir.nii.ac.jp/crid/2050307416982638848","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial and temporal characteristics of optimum process noise values of tropospheric parameters for kinematic analysis of Global Navigation Satellite System (GNSS) sites in Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588891959347456","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Source process with heterogeneous rupture velocity for the 2011 Tohoku-Oki earthquake based on 1-Hz GPS data"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892104447744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Real-time automatic uncertainty estimation of coseismic single rectangular fault model using GNSS data"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892106671616","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the performance of position-domain sidereal filter for 30-s kinematic GPS to mitigate multipath errors"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317036804096","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rapid and quantitative uncertainty estimation of coseismic slip distribution for large interplate earthquakes using real-time GNSS data and its application to tsunami inundation prediction"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317068482944","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic characteristics of very-high-rate GPS observations for seismology"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1084531"},{"@type":"CROSSREF","@value":"10.1186/bf03353070_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/bf03353372_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0578-y_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1038/srep00931_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0572-4_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.35_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01425-0_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.20965/jdr.2014.p0339_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.11.005_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01584-8_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01586-6_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/bf03351914_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.20965/jdr.2018.p0460_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1029/2011jb008750_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1186/bf03353077_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.1364/oe.23.00a428_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"},{"@type":"CROSSREF","@value":"10.20965/jdr.2018.p0453_references_DOI_NmUshdMgK7S3ffJfI1cPiZaMpiW"}]}