{"@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/1362825893694369792.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1213778"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1213778"}}],"dc:title":[{"@value":"Near-Field Deformation from the El Mayor–Cucapah Earthquake Revealed by Differential LIDAR"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Earthquakes from Above</jats:title>\n          <jats:p>\n            Preparing for risks and hazards associated with large earthquakes requires detailed understanding of their mechanical properties. In addition to pinpointing the location and magnitude of earthquakes, postmortem analyses of the extent of rupture and amount of deformation are key quantities, but are not simply available from seismological data alone. Using a type of optical remote sensing, Light Detection and Ranging (LiDAR),\n            <jats:bold>\n              Oskin\n              <jats:italic>et al.</jats:italic>\n            </jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" page=\"702\" related-article-type=\"in-this-issue\" vol=\"335\" xlink:href=\"10.1126/science.1213778\">702</jats:related-article>\n            ) surveyed the surrounding area that ruptured during the 2010\n            <jats:italic>M</jats:italic>\n            <jats:sub>w</jats:sub>\n            7.2 El Mayor–Cucapah earthquake in Northern Mexico. Because this area had also been analyzed in 2006, a comparative analysis revealed slip rate and strain release on the shallow fault zone and a number of previously unknown faults. As remote imaging becomes cheaper and more common, differential analyses will continue to provide fault-related deformation data that complements modern seismological networks.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382825893694369795","@type":"Researcher","foaf:name":[{"@value":"Michael E. Oskin"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, University of California, Davis, 1 Shields Avenue, Davis, CA 95618, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369921","@type":"Researcher","foaf:name":[{"@value":"J Ramon Arrowsmith"}],"jpcoar:affiliationName":[{"@value":"School of Earth and Space Exploration, Arizona State University, Tempe, AZ 85287–1404, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369797","@type":"Researcher","foaf:name":[{"@value":"Alejandro Hinojosa Corona"}],"jpcoar:affiliationName":[{"@value":"Centro de Investigación Científica y de Educación Superior de Ensenada, Carretera Ensenada-Tijuana no. 3918, Zona Playitas, C.P. 22860, Ensenada, Baja California, México."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369920","@type":"Researcher","foaf:name":[{"@value":"Austin J. Elliott"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, University of California, Davis, 1 Shields Avenue, Davis, CA 95618, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369798","@type":"Researcher","foaf:name":[{"@value":"John M. Fletcher"}],"jpcoar:affiliationName":[{"@value":"Centro de Investigación Científica y de Educación Superior de Ensenada, Carretera Ensenada-Tijuana no. 3918, Zona Playitas, C.P. 22860, Ensenada, Baja California, México."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369794","@type":"Researcher","foaf:name":[{"@value":"Eric J. Fielding"}],"jpcoar:affiliationName":[{"@value":"Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91109, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369799","@type":"Researcher","foaf:name":[{"@value":"Peter O. Gold"}],"jpcoar:affiliationName":[{"@value":"Department of Geology, University of California, Davis, 1 Shields Avenue, Davis, CA 95618, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369793","@type":"Researcher","foaf:name":[{"@value":"J. Javier Gonzalez Garcia"}],"jpcoar:affiliationName":[{"@value":"Centro de Investigación Científica y de Educación Superior de Ensenada, Carretera Ensenada-Tijuana no. 3918, Zona Playitas, C.P. 22860, Ensenada, Baja California, México."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369800","@type":"Researcher","foaf:name":[{"@value":"Ken W. Hudnut"}],"jpcoar:affiliationName":[{"@value":"United States Geological Survey, 525 South Wilson Avenue, Pasadena, CA 91106, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369796","@type":"Researcher","foaf:name":[{"@value":"Jing Liu-Zeng"}],"jpcoar:affiliationName":[{"@value":"National Key Laboratory of Earthquake Dynamics, Institute of Geology, China Earthquake Administration, 1# Huayanli, Dewai Avenue, Beijing 100029."}]},{"@id":"https://cir.nii.ac.jp/crid/1382825893694369792","@type":"Researcher","foaf:name":[{"@value":"Orlando J. Teran"}],"jpcoar:affiliationName":[{"@value":"Centro de Investigación Científica y de Educación Superior de Ensenada, Carretera Ensenada-Tijuana no. 3918, Zona Playitas, C.P. 22860, Ensenada, Baja California, México."}]}],"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":"2012-02-10","prism:volume":"335","prism:number":"6069","prism:startingPage":"702","prism:endingPage":"705"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1213778"}],"createdAt":"2012-02-09","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360002214585691136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatio‐temporal distribution of fault slip and high‐frequency radiation of the 2010 El Mayor‐Cucapah, Mexico earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360016864717825536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Irregular rupture propagation and geometric fault complexities during the 2010 Mw 7.2 El Mayor-Cucapah earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617572632448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Topographic Evolution Involving Co-Seismic Landslide, Deformation, Long-Term Folding and Isostatic Rebound: A Case Study on the 2004 Chuetsu Earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/1360306905605997440","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Geomorphologic mapping and analysis of fault activities along the northern margin of the Yanfan Basin, China"}]},{"@id":"https://cir.nii.ac.jp/crid/1360566399836905856","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Compact passively Q-switched single-frequency Er<sup>3+</sup>/Yb<sup>3+</sup>codoped phosphate fiber laser"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182122906368","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Detection of subtle tectonic–geomorphic features in densely forested mountains by very high-resolution airborne LiDAR survey"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848663120853504","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"3D Surface Displacement and Surface Ruptures Associated with the 2014 Mw 6.2 Nagano Earthquake Using Differential Lidar"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870366936052352","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Small-displacement linear surface ruptures of the 2016 Kumamoto earthquake sequence detected by ALOS-2 SAR interferometry"}]},{"@id":"https://cir.nii.ac.jp/crid/2051433317028471808","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Characteristics of secondary-ruptured faults in the Aso Caldera triggered by the 2016 Mw 7.0 Kumamoto earthquake"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1213778"},{"@type":"CROSSREF","@value":"10.1002/jgrb.50144_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1038/s41598-022-08671-6_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.3390/rs13061073_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2024.109568_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.7567/apex.10.052502_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1186/s40623-016-0534-x_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1016/j.geomorph.2012.11.001_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1186/s40623-020-01306-y_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"},{"@type":"CROSSREF","@value":"10.1785/0120180020_references_DOI_DIiUSv3dTccLPM36N9Orikwi2oq"}]}