{"@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/1363388845459128064.json","@type":"Article","productIdentifier":[{"identifier":{"@type":"DOI","@value":"10.1029/98jb00162"}},{"identifier":{"@type":"URI","@value":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JB00162"}},{"identifier":{"@type":"URI","@value":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JB00162"}}],"dc:title":[{"@value":"Quantitative measure of the variation in fault rheology due to fluid‐rock interactions"}],"description":[{"type":"abstract","notation":[{"@value":"<jats:p>We analyze friction data from two published suites of laboratory tests on granite in order to explore and quantify the effects of temperature (<jats:italic>T</jats:italic>) and pore water pressure (<jats:italic>P<jats:sub>p</jats:sub></jats:italic>) on the sliding behavior of faults. Rate‐stepping sliding tests were performed on laboratory faults in granite containing “gouge” (granite powder), both dry at 23° to 845°C [<jats:italic>Lockner et al.</jats:italic>, 1986], and wet (<jats:italic>P<jats:sub>p</jats:sub></jats:italic> = 100 MPa) at 23° to 600°C [<jats:italic>Blanpied et al</jats:italic>., 1991, 1995]. Imposed slip velocities (<jats:italic>V</jats:italic>) ranged from 0.01 to 5.5 μm/s, and effective normal stresses were near 400 MPa. For dried granite at all temperatures, and wet granite below ∼300°C, the coefficient of friction (μ) shows low sensitivity to <jats:italic>V</jats:italic>, <jats:italic>T</jats:italic>, and <jats:italic>P<jats:sub>p</jats:sub></jats:italic>. For wet granite above ∼350°, μ drops rapidly with increasing <jats:italic>T</jats:italic> and shows a strong, positive rate dependence and protracted strength transients following steps in <jats:italic>V</jats:italic>, presumably reflecting the activity of a water‐aided deformation process. By inverting strength data from velocity stepping tests we determined values for parameters in three formulations of a rate‐ and state‐dependent constitutive law. One or two state variables were used to represent slip history effects. Each velocity step yielded an independent set of values for the nominal friction level, five constitutive parameters (transient parameters <jats:italic>a</jats:italic>, <jats:italic>b</jats:italic><jats:sub>1</jats:sub>, and <jats:italic>b</jats:italic><jats:sub>2</jats:sub> and characteristic displacements <jats:italic>D<jats:sub>c1</jats:sub></jats:italic> and <jats:italic>D<jats:sub>c2</jats:sub></jats:italic>), and the velocity dependence of steady state friction ∂μ<jats:sub>ss</jats:sub>/∂ ln <jats:italic>V</jats:italic> = <jats:italic>a</jats:italic>‐<jats:italic>b</jats:italic><jats:sub>1</jats:sub>−<jats:italic>b</jats:italic><jats:sub>2</jats:sub>. Below 250°, data from dry and most wet tests are adequately modeled by using the “slip law” [<jats:italic>Ruina</jats:italic>, 1983] and one state variable (<jats:italic>a</jats:italic> = 0.003 to 0.018, <jats:italic>b</jats:italic> = 0.001 to +0.018, <jats:italic>D<jats:sub>c</jats:sub></jats:italic> ≈ 1 to 20 μm). Dried tests above 250° can also be fitted with one state variable. In contrast, wet tests above 350° require higher direct rate dependence (<jats:italic>a</jats:italic> = 0.03 to 0.12), plus a second state variable with large, negative amplitude (<jats:italic>b</jats:italic><jats:sub>2</jats:sub> = −0.03 to −0.14) and large characteristic displacement (<jats:italic>D</jats:italic><jats:sub>c2</jats:sub> = 300 to >4000 μm). Thus the parameters <jats:italic>a</jats:italic>, <jats:italic>b</jats:italic><jats:sub>1</jats:sub>, and <jats:italic>b</jats:italic><jats:sub>2</jats:sub> for wet granite show a pronounced change in their temperature dependence in the range 270° to 350°C, which may reflect a change in underlying deformation mechanism. We quantify the trends in parameter values from 25° to 600°C by piecewise linear regressions, which provide a straightforward means to incorporate the full constitutive response of granite into numerical models of fault slip. The modeling results suggest that the succeptibility for unstable (stick‐slip) sliding is maximized between 90° and 360°C, in agreement with laboratory observations and consistent with the depth range of earthquakes on mature faults in the continental crust.</jats:p>"}]}],"creator":[{"@id":"https://cir.nii.ac.jp/crid/1380004054074789506","@type":"Researcher","foaf:name":[{"@value":"M. L. Blanpied"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845459128068","@type":"Researcher","foaf:name":[{"@value":"C. J. Marone"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845459128064","@type":"Researcher","foaf:name":[{"@value":"D. A. Lockner"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845459128065","@type":"Researcher","foaf:name":[{"@value":"J. D. Byerlee"}]},{"@id":"https://cir.nii.ac.jp/crid/1383388845459128067","@type":"Researcher","foaf:name":[{"@value":"D. P. King"}]}],"publication":{"publicationIdentifier":[{"@type":"PISSN","@value":"01480227"}],"prism:publicationName":[{"@value":"Journal of Geophysical Research: Solid Earth"}],"dc:publisher":[{"@value":"American Geophysical Union (AGU)"}],"prism:publicationDate":"1998-05-10","prism:volume":"103","prism:number":"B5","prism:startingPage":"9691","prism:endingPage":"9712"},"reviewed":"false","dc:rights":["http://onlinelibrary.wiley.com/termsAndConditions#vor"],"url":[{"@id":"https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1029%2F98JB00162"},{"@id":"https://agupubs.onlinelibrary.wiley.com/doi/pdf/10.1029/98JB00162"}],"createdAt":"2004-02-03","modifiedAt":"2023-09-22","relatedProduct":[{"@id":"https://cir.nii.ac.jp/crid/1050001202560213760","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Spectrum of slip behaviour in Tohoku fault zone samples at plate tectonic slip rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1050022457828784768","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Implementation into earthquake sequence simulations of a rate- and state-dependent friction law incorporating pressure solution creep"}]},{"@id":"https://cir.nii.ac.jp/crid/1050285700281570048","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Depth dependence of the frictional behavior of montmorillonite fault gouge: Implications for seismicity along a décollement zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1050303932805499904","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Homoclinic bifurcation of a rate-weakening patch in a viscoelastic medium and effect of strength contrast"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214349012992","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Under what circumstances does a seismogenic patch produce aseismic transients in the later interseismic period?"}]},{"@id":"https://cir.nii.ac.jp/crid/1360002214351275136","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional properties of JFAST core samples and implications for slow earthquakes at the Tohoku subduction zone"}]},{"@id":"https://cir.nii.ac.jp/crid/1360004233287238784","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"On the transient response of serpentine (antigorite) gouge to stepwise changes in slip velocity under high-temperature conditions"}]},{"@id":"https://cir.nii.ac.jp/crid/1360009142776325376","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Effect of normal stress on the frictional behavior of brucite: application to slow earthquakes at the subduction plate  interface in the mantle wedge"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017279830000256","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Extension of Aseismic Slip Propagation Theory to Slow Earthquake Migration"}]},{"@id":"https://cir.nii.ac.jp/crid/1360017282189457792","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Segmentation of Shallow Slow Slip Events at the Hikurangi Subduction Zone Explained by Along‐Strike Changes in Fault Geometry and Plate Convergence Rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283690387835648","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The detectability of shallow slow earthquakes by the Dense Oceanfloor Network system for Earthquakes and Tsunamis (DONET) in Tonankai district, Japan"}]},{"@id":"https://cir.nii.ac.jp/crid/1360283692753666432","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Earthquake sequence simulations with measured properties for JFAST core samples"}]},{"@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/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/1360298757434042112","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"The evolution of rock friction is more sensitive to slip than elapsed time, even at near-zero slip rates"}]},{"@id":"https://cir.nii.ac.jp/crid/1360302866832813696","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Tertiary creep behavior for various rate- and state-dependent friction laws"}]},{"@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/1360567179757322752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Velocity‐ and slip‐dependent weakening in simulated fault gouge: Implications for multimode fault slip"}]},{"@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/1360848654735701120","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Shear localization in a mature mylonitic rock analog during fast slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360861707357240576","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Spatial Patterns in Frictional Behavior of Sediments Along the Kumano Transect in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869454549520128","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A physical explanation for an unusually long-duration slow slip event in the Nankai Trough"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869854370617472","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Community‐Driven Code Comparisons for Simulations of Fluid‐Induced Aseismic Slip"}]},{"@id":"https://cir.nii.ac.jp/crid/1360869856056522752","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Reconciling aging and slip state evolutions from laboratory-derived canons of rate-and-state friction"}]},{"@id":"https://cir.nii.ac.jp/crid/1361131418080191232","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Seismological Investigations of Induced Earthquakes Near the Hutubi Underground Gas Storage Facility"}]},{"@id":"https://cir.nii.ac.jp/crid/1361694368033642240","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"First‐principles Investigation of Frictional Characteristics of Brucite: An Application to Its Macroscopic Frictional Characteristics"}]},{"@id":"https://cir.nii.ac.jp/crid/1390001204303058688","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Mechanisms for Variation in Size and Occurrence Interval of Interplate Earthquakes"},{"@language":"ja","@value":"プレート境界地震の規模と発生間隔変化のメカニズム"}]},{"@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/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/1390282681490622208","@type":"Article","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@language":"en","@value":"Seismic cycle on a strike-slip fault with rate- and state-dependent strength in an elastic layer overlying a viscoelastic half-space"}]},{"@id":"https://cir.nii.ac.jp/crid/1520291855129630208","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Migration process of very low-frequency events based on a chain-reaction model and its application to the detection of preseismic slip for megathrust earthquakes"}]},{"@id":"https://cir.nii.ac.jp/crid/2050025942151020672","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Frictional stability of porous tuff breccia under subsurface pressure conditions and implications for shallow seismicity"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892108505088","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"Dynamic earthquake sequence simulation with an SBIEM accounting for interseismic poroelastic rebound"}]},{"@id":"https://cir.nii.ac.jp/crid/2050588892138322688","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A possible mechanism of M 9 earthquake generation cycles in the area of repeating M 7～8 earthquakes surrounded by aseismic sliding"}]},{"@id":"https://cir.nii.ac.jp/crid/2051714792046925952","@type":"Article","resourceType":"学術雑誌論文(journal article)","relationType":["isReferencedBy"],"jpcoar:relatedTitle":[{"@value":"A trial derivation of seismic plate coupling by focusing on the activity of shallow slow earthquakes"}]}],"dataSourceIdentifier":[{"@type":"CROSSREF","@value":"10.1029/98jb00162"},{"@type":"CROSSREF","@value":"10.1002/2014gl061676_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2017gl073460_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2010jb008062_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.5194/se-12-171-2021_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/s40623-021-01419-y_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2021jb023800_references_DOI_86KrYFEaQpyhX7HvL9v7w2F4ymY"},{"@type":"CROSSREF","@value":"10.1029/2021jb022913_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1007/s11001-013-9192-6_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1038/ngeo2547_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1098/rsta.2016.0003_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.5047/eps.2010.09.003_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2014jb011170_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2017gl074307_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1093/gji/ggw058_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.391_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2011.08.012_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1073/pnas.2119462119_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1016/j.epsl.2023.118314_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1016/j.tecto.2024.230439_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2017gl073465_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/bf03353322_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2015gl065829_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/1880-5981-66-55_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.4294/zisin.61.415_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/bf03353305_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.5047/eps.2011.06.022_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1002/2016gc006687_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2021jb022546_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/s40623-022-01649-8_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2024jb030601_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1186/s40623-024-02100-w_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1093/gji/ggae464_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2019jb017360_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1029/2019jb017740_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"},{"@type":"CROSSREF","@value":"10.1016/j.jsg.2011.12.001_references_DOI_MTzVFyBX3ZB2KxwWAsvFFR5btdA"}]}