{"@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/1361137045269348992.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1113746"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1113746"}}],"dc:title":[{"@value":"The Size and Duration of the Sumatra-Andaman Earthquake from Far-Field Static Offsets"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>\n            The 26 December 2004 Sumatra earthquake produced static offsets at continuously operating GPS stations at distances of up to 4500 kilometers from the epicenter. We used these displacements to model the earthquake and include consideration of the Earth's shape and depth-varying rigidity. The results imply that the average slip was >5 meters along the full length of the rupture, including the ∼650-kilometer-long Andaman segment. Comparison of the source derived from the far-field static offsets with seismically derived estimates suggests that 25 to 35% of the total moment release occurred at periods greater than 1 hour. Taking into consideration the strong dip dependence of moment estimates, the magnitude of the earthquake did not exceed\n            <jats:italic>M</jats:italic>\n            <jats:sub>w</jats:sub>\n            = 9.2.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004054083349653","@type":"Researcher","foaf:name":[{"@value":"P. Banerjee"}],"jpcoar:affiliationName":[{"@value":"Wadia Institute of Himalayan Geology, Dehra Dun, 248001, India."},{"@value":"U.S. Geological Survey, Menlo Park, CA 94025, USA."},{"@value":"Department of Earth and Planetary Science and Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045269348993","@type":"Researcher","foaf:name":[{"@value":"F. F. Pollitz"}],"jpcoar:affiliationName":[{"@value":"Wadia Institute of Himalayan Geology, Dehra Dun, 248001, India."},{"@value":"U.S. Geological Survey, Menlo Park, CA 94025, USA."},{"@value":"Department of Earth and Planetary Science and Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381137045269348992","@type":"Researcher","foaf:name":[{"@value":"R. Bürgmann"}],"jpcoar:affiliationName":[{"@value":"Wadia Institute of Himalayan Geology, Dehra Dun, 248001, India."},{"@value":"U.S. Geological Survey, Menlo Park, CA 94025, USA."},{"@value":"Department of Earth and Planetary Science and Berkeley Seismological Laboratory, University of California, Berkeley, CA 94720, 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":"2005-06-17","prism:volume":"308","prism:number":"5729","prism:startingPage":"1769","prism:endingPage":"1772"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1113746"}],"createdAt":"2005-05-20","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050282810779206656","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low-frequency acoustic-gravity waves from coseismic vertical deformation associated with the 2004 Sumatra-Andaman earthquake (Mw=9.2)"},{"@value":"Low‐frequency acoustic‐gravity waves from coseismic vertical deformation associated with the 2004 Sumatra‐Andaman earthquake (<i>M</i><sub><i>w</i></sub> = 9.2)"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004231143607168","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Radiated Energy of Great Earthquakes from Teleseismic Empirical Green’s Function Deconvolution"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004232523316480","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Analysis of the far-field crustal displacements caused by the 2011 Great Tohoku earthquake inferred from continuous GPS observations"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166662239232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Ionospheric electron enhancement preceding the 2011 Tohoku-Oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565168391791488","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A Tale of Two Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640349255936","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Postseismic relaxation due to Bhuj earthquake on January 26, 2001: possible mechanisms and processes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848659520058880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spectral-finite element approach to post-seismic relaxation in a spherical compressible Earth: application to gravity changes due to the 2004 Sumatra–Andaman earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511780608","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Differences in tsunami generation between the December 26, 2004 and March 28, 2005 Sumatra earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511781888","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Global deformation from the great 2004 Sumatra-Andaman Earthquake observed by GPS: Implications for rupture process and global reference frame"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206511783040","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Global co-seismic displacements caused by the 2004 Sumatra-Andaman earthquake (Mw 9.1)"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512475392","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Outline of vertical displacement of the 2004 and 2005 Sumatra earthquakes revealed by satellite radar imagery"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367115171968","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Contemporary horizontal crustal movement estimation for northwestern Vietnam inferred from repeated GPS 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