{"@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/1363388843393647872.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.1139763"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.1139763"}},{"identifier":{"@type":"PMID","@value":"17495160"}}],"dc:title":[{"@value":"Ultralow Friction of Carbonate Faults Caused by Thermal Decomposition"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>High-velocity weakening of faults may drive fault motion during large earthquakes. Experiments on simulated faults in Carrara marble at slip rates up to 1.3 meters per second demonstrate that thermal decomposition of calcite due to frictional heating induces pronounced fault weakening with steady-state friction coefficients as low as 0.06. Decomposition produces particles of tens of nanometers in size, and the ultralow friction appears to be associated with the flash heating on an ultrafine decomposition product. Thus, thermal decomposition may be an important process for the dynamic weakening of faults.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1383388843393647873","@type":"Researcher","foaf:name":[{"@value":"Raehee Han"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea."},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan."},{"@value":"Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843393647874","@type":"Researcher","foaf:name":[{"@value":"Toshihiko Shimamoto"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea."},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan."},{"@value":"Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843393647872","@type":"Researcher","foaf:name":[{"@value":"Takehiro Hirose"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea."},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan."},{"@value":"Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843393647875","@type":"Researcher","foaf:name":[{"@value":"Jin-Han Ree"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea."},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan."},{"@value":"Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan."}]},{"@id":"https://cir.nii.ac.jp/crid/1383388843393647876","@type":"Researcher","foaf:name":[{"@value":"Jun-ichi Ando"}],"jpcoar:affiliationName":[{"@value":"Department of Earth and Environmental Sciences, Korea University, Seoul 136-701, South Korea."},{"@value":"Division of Earth and Planetary Sciences, Graduate School of Science, Kyoto University, Kyoto 606-8502, Japan."},{"@value":"Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan."}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"00368075"},{"@type":"EISSN","@value":"10959203"},{"@type":"PISSN","@value":"https://id.crossref.org/issn/00368075"}],"prism:publicationName":[{"@value":"Science"}],"dc:publisher":[{"@value":"American Association for the Advancement of Science (AAAS)"}],"prism:publicationDate":"2007-05-11","prism:volume":"316","prism:number":"5826","prism:startingPage":"878","prism:endingPage":"881"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.1139763"}],"createdAt":"2007-05-10","modifiedAt":"2024-01-10","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001335764454144","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Coseismic dehydration of serpentinite: Evidence from high-velocity friction experiments"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022543170350336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Relationship of evolution of slip-surface structure in Indian sandstone to changes in friction coefficient for a wide range of slip 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