{"@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/1362262944084880000.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1235637"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1235637"}}],"dc:title":[{"@value":"From Sub-Rayleigh to Supershear Ruptures During Stick-Slip Experiments on Crustal Rocks"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Sonic Boom from Below</jats:title>\n          <jats:p>\n            Seismic shear waves released by an earthquake typically far outpace motion along the fault surface. Occasionally, however, earthquakes along strike-slip faults appear to propagate so that the rupture velocity is faster than shear waves, creating a sort of sonic boom along the fault surface.\n            <jats:bold>\n              Passelègue\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\" issue=\"6137\" page=\"1208\" related-article-type=\"in-this-issue\" vol=\"340\" xlink:href=\"10.1126/science.1235637\">1208</jats:related-article>\n            ) were able to reproduce and measure these so-called supershear ruptures in stick-slip experiments with two pieces of granite under high applied normal stress. Much like during a sonic boom when a plane travels faster than the speed of sound, the ruptures created a shock wave in the form of a Mach cone around the rupture front.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1382262944084880003","@type":"Researcher","foaf:name":[{"@value":"François X. Passelègue"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, CNRS UMR 8538, École Normale Supérieure, 75005 Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944084880000","@type":"Researcher","foaf:name":[{"@value":"Alexandre Schubnel"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, CNRS UMR 8538, École Normale Supérieure, 75005 Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944084880004","@type":"Researcher","foaf:name":[{"@value":"Stefan Nielsen"}],"jpcoar:affiliationName":[{"@value":"Istituto Nazionale di Geofisica e Vulcanologia, Roma 00143, Italy."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944084880001","@type":"Researcher","foaf:name":[{"@value":"Harsha S. Bhat"}],"jpcoar:affiliationName":[{"@value":"Institut de Physique du Globe de Paris, 1 rue Jussieu, 75238 cedex 05 Paris, France."}]},{"@id":"https://cir.nii.ac.jp/crid/1382262944084880002","@type":"Researcher","foaf:name":[{"@value":"Raùl Madariaga"}],"jpcoar:affiliationName":[{"@value":"Laboratoire de Géologie, CNRS UMR 8538, École Normale Supérieure, 75005 Paris, France."}]}],"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":"2013-06-07","prism:volume":"340","prism:number":"6137","prism:startingPage":"1208","prism:endingPage":"1211"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1235637"}],"createdAt":"2013-06-06","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004232523514496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Strain rate effect on fault slip and rupture evolution: Insight from meter-scale rock friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233292309632","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Robust Estimation of Rupture Properties at Propagating Front of Laboratory Earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360298755638923136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"High-pressure shock compression of olivine: Dynamic pulverization and frictional melting"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848657453648768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatiotemporal complexity of 2-D rupture nucleation process observed by direct monitoring during large-scale biaxial rock friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1390285300159441280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Subsonic to intersonic transition in sliding friction of soft solids"},{"@language":"ja","@value":"柔らかい固体のすべり接触における亜音速-超音速遷移"},{"@value":"Subsonic to Intersonic Transition in Sliding Friction for Soft Solids"}]},{"@id":"https://cir.nii.ac.jp/crid/1390564238108729600","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Probing Earthquake Physics Using Multidisciplinary Approaches"},{"@language":"ja","@value":"分野横断的なアプローチを用いた地震の物理の研究"},{"@language":"ja-Kana","@value":"ブンヤ オウダンテキ ナ アプローチ オ モチイタ ジシン ノ ブツリ ノ ケンキュウ"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892141558400","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of stress state on slow rupture propagation in synthetic fault gouges"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1235637"},{"@type":"CROSSREF","@value":"10.1029/2018jb016797_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.1103/physrevlett.124.238001_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.1016/j.pepi.2023.107009_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0199-x_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.11.039_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.4294/zisin.2018-12_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2017.12.023_references_DOI_IgnyHBYSOosEe7fVXhptC5Vh4qX"}]}