{"@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/1361981469967614336.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1126/science.231.4739.711"}},{"identifier":{"@type":"URI","@value":"https://www.science.org/doi/pdf/10.1126/science.231.4739.711"}}],"dc:title":[{"@value":"Transition Between Frictional Slip and Ductile Flow for Halite Shear Zones at Room Temperature"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>A complete transition from frictional slip to ductile shearing flow upon decreasing velocity (or slip rate) or increasing confining pressure is documented for a thin layer of halite undergoing large shearing deformation. The results indicate that the logarithmic law for steady-state friction with a negative velocity dependence breaks down when friction becomes nearly equal to the shear resistance required for ductile flow and that the law changes into a flow law in shear upon further decrease in velocity. The friction-velocity relation is crucial in stability analyses of fault motion, and the results are important for earthquake and state-of-stress problems, especially in the application of laboratory data to the slow average motion of natural faults and to the behavior of deep faults along which ductile deformation becomes increasingly predominant.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1381981469967614336","@type":"Researcher","foaf:name":[{"@value":"Toshihiko Shimamoto"}],"jpcoar:affiliationName":[{"@value":"Center for Tectonophysics, Texas A&M University, College Station 77843."}]}],"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":"1986-02-14","prism:volume":"231","prism:number":"4739","prism:startingPage":"711","prism:endingPage":"714"},"reviewed":"false","url":[{"@id":"https://www.science.org/doi/pdf/10.1126/science.231.4739.711"}],"createdAt":"2006-10-05","modifiedAt":"2024-01-12","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050303932805480960","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"The effective stress law at a brittle-plastic transition with a halite gouge layer"},{"@value":"The effective stress law at a brittle‐plastic transition with a halite gouge layer"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932805502336","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Comminution-Induced Transient Frictional Behavior in Sheared Granular Halite"},{"@value":"Comminution‐Induced Transient Frictional Behavior in Sheared Granular Halite"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932805506432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Fully dynamic earthquake sequence simulation of a fault in a viscoelastic medium using a spectral boundary integral equation method: does interseismic stress relaxation promote aseismic transients?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214348544768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Focal mechanisms of deep low‐frequency earthquakes in Eastern Shimane in Western Japan"}]},{"@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/1360285704779166464","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A friction to flow constitutive law and its application to a 2‐D modeling of earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360285710037210496","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Statistical physics of fracture, friction, and earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565165998088832","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Transient behavior and stability analyses of halite shear zones with an empirical rate-and-state friction to flow law"}]},{"@id":"https://cir.nii.ac.jp/crid/1360565166660677376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling the activity of short‐term slow slip events along deep subduction interfaces beneath Shikoku, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360567182476769152","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tectonic, volcanic, and semi-volcanic deep low-frequency earthquakes in western Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360580229830515712","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modifications of epidemic-type-aftershock-sequence models for characterizing diffusive shear slips of deep long-period earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/1360846640974802176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional properties of megathrust fault gouges at low sliding velocities: New data on effects of normal stress and temperature"}]},{"@id":"https://cir.nii.ac.jp/crid/1360848658219042176","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Modeling of slow slip events along the deep subduction zone in the Kii Peninsula and Tokai regions, southwest Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869855136952320","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Fault‐Valve Instability: A Mechanism for Slow Slip Events"}]},{"@id":"https://cir.nii.ac.jp/crid/1361412893056974592","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Three‐Dimensional Modeling of Spontaneous and Triggered Slow‐Slip Events at the Hikurangi Subduction Zone, New Zealand"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001206512270080","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling slips and nucleation processes at the deeper part of the seismogenic zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1390004222631008640","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Dynamic Earthquake Cycle Simulations Considering Changes in Dominant Deformation Mechanisms of a Fault Slip"},{"@language":"ja","@value":"断層滑りの支配的な変形機構の遷移を考慮に入れた動的地震サイクルシミュレーション"},{"@language":"ja-Kana","@value":"ダンソウ スベリ ノ シハイテキ ナ ヘンケイ キコウ ノ センイ オ コウリョ ニ イレタ ドウテキ ジシン サイクルシミュレーション"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282679279770240","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling Slow Slip Events at the Deeper Subduction Interfaces"},{"@language":"ja","@value":"沈み込み帯深部で発生するスロースリップイベントのモデル化"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681213934976","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Afterslip associated with interplate earthquakes and the viscoelastic behavior of rocks"},{"@language":"ja","@value":"プレート境界地震に伴う余効すべりと岩石の粘弾性挙動"},{"@language":"ja-Kana","@value":"プレート キョウカイ ジシン ニ トモナウ ヨコウスベリ ト ガンセキ ノ ネンダンセイ キョドウ"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681488766720","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Modeling slip processes at the deeper part of the seismogenic zone using a constitutive law combining friction and flow laws"}]},{"@id":"https://cir.nii.ac.jp/crid/1390282681489279744","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"A smeared seismicity constitutive model"},{"@language":"ja-Kana","@value":"smeared seismicity constitutive model"}]},{"@id":"https://cir.nii.ac.jp/crid/1390292706071091584","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Low-frequency Earthquakes in the Continental Plate and Their Seismological and Tectonic Implications"},{"@language":"ja","@value":"陸域下の低周波地震とその地震学的およびテクトニクス的意義"}]},{"@id":"https://cir.nii.ac.jp/crid/1390870529360675456","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"ja","@value":"脆性–塑性遷移領域における岩石の変形と水の効果について"},{"@language":"en","@value":"Effects of Water on the Deformation of Rocks at the Brittle–Plastic Transition: Insight from High-pressure and High-temperature Deformation Experiment on Quartz + Water Aggregates"},{"@value":"脆性-塑性遷移領域における岩石の変形と水の効果について : 石英多結晶体の高含水変形実験からの知見"},{"@language":"ja-Kana","@value":"ゼイセイ-ソセイ センイ リョウイキ ニ オケル ガンセキ ノ ヘンケイ ト ミズ ノ コウカ ニ ツイテ : セキエイ タケッショウタイ ノ コウガンスイ ヘンケイ ジッケン カラ ノ チケン"}]},{"@id":"https://cir.nii.ac.jp/crid/2050870367116798080","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Rheological profile across the NE Japan interplate megathrust in the source region of the 2011 Mw9.0 Tohoku-oki earthquake"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046945536","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Along-strike variations in temperature and tectonic tremor activity along the Hikurangi subduction zone, New Zealand"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1126/science.231.4739.711"},{"@type":"CROSSREF","@value":"10.1002/2013jb010681_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1002/2015gl067544_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/s40623-014-0142-6_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2012.12.015_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2020gc009165_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.5026/jgeography.131.289_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-73_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1002/2014jb011170_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1103/revmodphys.84.839_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.5026/jgeography.129.491_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2011.08.012_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2008jb006057_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/bf03353322_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/bf03353327_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.5575/geosoc.115.448_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.415_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1093/gji/ggad125_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/bf03353331_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2011jb009083_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2024jb029165_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2024gl109645_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.5026/jgeography.135.33_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1029/2019jb018190_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1186/s40623-019-1113-8_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2011.12.001_references_DOI_M1iSI9gOKePtJB3Bqn1bdy6UigN"}]}