Effects of humidity and interlayer cations on the frictional strength of montmorillonite
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- Material Type
- 記事
- Author/Editor
- Hiroshi TetsukaIkuo KatayamaHiroshi Sakuma
- Publication, Distribution, etc.
- Publication Date
- 2018-04-10
- Publication Date (W3CDTF)
- 2018-04-10
- Periodical title
- EPS : Earth, Planets and Space
- No. or year of volume/issue
- 70(56)
- Volume
- 70(56)
- ISSN (Periodical Title)
- 1880-5981
- ISSN-L (Periodical Title)
- 1343-8832
- Text Language Code
- eng
- DOI
- 10.1186/s40623-018-0829-1
- Persistent ID (NDL)
- info:ndljp/pid/11125823
- Collection
- Collection (Materials For Handicapped People:1)
- Collection (particular)
- 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- Acquisition Basis
- オンライン資料収集制度
- Date Accepted (W3CDTF)
- 2018-08-10T20:26:03+09:00
- Date Captured (W3CDTF)
- 2018-08-10
- Format (IMT)
- application/pdf
- Access Restrictions
- 国立国会図書館内限定公開
- Service for the Digitized Contents Transmission Service
- 図書館・個人送信対象外
- Availability of remote photoduplication service
- 可
- Periodical Title (URI)
- Periodical Title (Persistent ID (NDL))
- info:ndljp/pid/11067456
- Data Provider (Database)
- 国立国会図書館 : 国立国会図書館デジタルコレクション
- Summary, etc.
- コレクション : 国立国会図書館デジタルコレクション > 電子書籍・電子雑誌 > その他
- DOI
- 10.1186/s40623-018-0829-1
- Access Restrictions
- インターネット公開
- Related Material (URI)
- Is Referenced By
- Friction in clay-bearing faults increases with the ionic radius of interlayer cationsA small amount of water reduces the friction of the preferentially oriented montmorillonite gougeWhat is the origin of macroscopic friction?Potential Role of Volcanic Glass‐Smectite Mixtures in Slow Earthquakes in Shallow Subduction Zones: Insights From Low‐ to High‐Velocity Friction ExperimentsInterlayer energy of pyrophyllite: Implications for macroscopic frictionDepth profile of frictional properties in the inner Nankai accretionary prism using cuttings from IODP Site C0002Sensitivity of elastic thickness to water in the Martian lithosphereInelastic behavior and mechanical strength of the shallow upper crust controlled by layer-parallel slip in the high-strain zone of the Niigata region, JapanStrength models of the terrestrial planets and implications for their lithospheric structure and evolution
- References
- Dynamic weakening of smectite‐bearing faults at intermediate velocities: Implications for subduction zone earthquakesStuck in the mud? Earthquake nucleation and propagation through accretionary forearcsPelagic smectite as an important factor in tsunamigenic slip along the Japan TrenchOrigin and significance of clay‐coated fractures in mudrock fragments of the SAFOD borehole (Parkfield, California)Abundance of smectite and the location of a plate-boundary fault, Barbados accretionary prismLaboratory results indicating complex and potentially unstable frictional behavior of smectite clayMineralogy and physical nature of clay gougeShear zones in clay-rich fault gouge: A laboratory study of fabric development and evolutionMineralogical characterization of protolith and fault rocks from the SAFOD Main HoleClay gougeInterlayer bonding energy of layered minerals: Implication for the relationship with friction coefficientFrictional characteristics of single and polycrystalline muscovite and influence of fluid chemistry3. Sediment Inputs to Subduction ZonesAn experimental investigation into the role of phyllosilicate content on earthquake propagation during seismic slip in carbonate faultsPermeability and frictional strength of cation‐exchanged montmorilloniteSummary of results of frictional sliding studies, at confining pressures up to 6.98 kb, in selected rock materialsEffect of clay content and mineralogy on frictional sliding behavior of simulated gouges: Binary and ternary mixtures of quartz, illite, and montmorilloniteHydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gougeSwelling behavior of Na- and Ca-montmorillonite up to 150°C by <i>in situ</i> X-Ray diffraction experiments11. Friction of the Smectite Clay MontmorilloniteThe effect of mineral bond strength and adsorbed water on fault gouge frictional strengthSwelling Properties of Montmorillonite and Beidellite Clay Minerals from Molecular Simulation: Comparison of Temperature, Interlayer Cation, and Charge Location EffectsClay mineral anomalies in the fault zone of the Chelungpu Fault, Taiwan, and their implicationsLaboratory observations of time‐dependent frictional strengthening and stress relaxation in natural and synthetic fault gougesConstitutive properties of clayey fault gouge from the Hanaore fault zone, southwest JapanAdsorption of Water Vapor by Montmorillonite. II. Effect of Exchangeable Ions and Lattice Swelling as Measured by X-Ray DiffractionEffects of clay content on the frictional strength and fluid transport property of faultsEffect of hydration state on the frictional properties of montmorillonite‐based fault gougeThe shearing behaviour of claysFrictional dependence of gouge mixtures of quartz and montmorillonite on velocity, composition and fabricFault rocks and past to recent fluid characteristics from the borehole survey of the Nojima fault ruptured in the 1995 Kobe earthquake, southwest JapanFrictional strength of wet and dry montmorilloniteComparison of smectite- and illite-rich gouge frictional properties: application to the updip limit of the seismogenic zone along subduction megathrustsWater films at grain-grain contacts: Debye-Hückel, osmotic model of stress, salinity, and mineralogy dependenceA note on the effect of fault gouge composition on the stability of frictional slidingOn the Cation Dependence of Interlamellar and Interparticular Water and Swelling in Smectite ClaysCrystallographic controls on the frictional behavior of dry and water‐saturated sheet structure mineralsThe drained residual strength of cohesive soilsFriction of rocksEffects of simulated clay gouges on the sliding behavior of Tennessee sandstonThe effect of mineralogy and effective normal stress on frictional strength of sheet silicatesCompositional and fluid pressure controls on the state of stress on the Nankai subduction thrust: A weak plate boundaryEffect of temperature on the frictional behavior of smectite and illite
- Data Provider (Database)
- 国立情報学研究所 : CiNii Research
- Original Data Provider (Database)
- 雑誌記事索引データベースCrossref科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベース科学研究費助成事業データベースCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossrefCrossref
- Bibliographic ID (NDL)
- 11125823