{"@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/1361137044364045312.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1239577"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1239577"}}],"dc:title":[{"@value":"Slow Earthquakes, Preseismic Velocity Changes, and the Origin of Slow Frictional Stick-Slip"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:title>Slow Stick-Slip</jats:title>\n          <jats:p>\n            While the character of slow earthquakes has been approximated for some time, precise slip histories and the underlying mechanisms have remained elusive.\n            <jats:bold>Kaproth and Marone</jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http://www.w3.org/1999/xlink\" ext-link-type=\"doi\" issue=\"6151\" page=\"1229\" related-article-type=\"in-this-issue\" vol=\"341\" xlink:href=\"10.1126/science.1239577\">1229</jats:related-article>\n            ; published online 15 August) have made laboratory observations of repetitive, slow stick-slip in fault-zone materials and developed a mechanical explanation for how earthquake-like dynamic slip nucleation could start and then arrest so as to produce slow slip. As preseismic slip is a precursor to rupture, temporal variations in elastic wave speeds should be monitored in regions of high seismic hazard.\n          </jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381137044364045313","@type":"Researcher","foaf:name":[{"@value":"Bryan M. Kaproth"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences, and Energy Institute Center for Geomechanics, Geofluids and Geohazards, Pennsylvania State University, University Park, PA 16802, USA."}]},{"@id":"https://cir.nii.ac.jp/crid/1381137044364045312","@type":"Researcher","foaf:name":[{"@value":"C. Marone"}],"jpcoar:affiliationName":[{"@value":"Department of Geosciences, and Energy Institute Center for Geomechanics, Geofluids and Geohazards, Pennsylvania State University, University Park, PA 16802, 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":"2013-09-13","prism:volume":"341","prism:number":"6151","prism:startingPage":"1229","prism:endingPage":"1232"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1239577"}],"createdAt":"2013-08-16","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1360004233292223744","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquakes and Tremor Linked to Seamount Subduction During Shallow Slow Slip at the Hikurangi Margin, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142705494528","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow Stick‐Slip Failure in Halite Gouge Caused by Brittle‐Plastic Fault Heterogeneity"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704778817280","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Slow stick slip of antigorite serpentinite under hydrothermal conditions as a possible mechanism for slow earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285704784584448","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Coseismic slip propagation on the Tohoku plate boundary fault facilitated by slip‐dependent weakening during slow fault slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360290617400394880","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Deep slow-slip events promote seismicity in northeastern Japan megathrust"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302865743074304","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effects of phyllosilicate content on the slip behavior of fault gouge: Insights from room-temperature friction experiments on quartz–talc mixtures"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368032268160","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismicity at the Northern Hikurangi Margin, New Zealand, and Investigation of the Potential Spatial and Temporal Relationships With a Shallow Slow Slip Event"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679213864576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"蛇紋岩の力学的性質とそのテクトニックな意義"},{"@language":"en","@value":"Rheological Properties of Serpentinite and Their Tectonic Significance"},{"@language":"ja-Kana","@value":"ジャモンガン ノ リキガクテキ セイシツ ト ソノ テクトニック ナ イギ"}]},{"@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"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046932736","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Non-volcanic seismic swarm and fluid transportation driven by subduction of the Philippine Sea slab beneath the Kii Peninsula, Japan"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.1239577"},{"@type":"CROSSREF","@value":"10.1029/2018jb016136_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-86_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1029/2020gc009165_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1002/2014gl062735_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1002/2017gl074307_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2020.116261_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2023.229845_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1186/s40623-015-0199-x_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.5026/jgeography.124.371_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"},{"@type":"CROSSREF","@value":"10.1029/2018jb017211_references_DOI_WRlwvBJGGULdFRnD0uRtw8HbVxd"}]}