The DOI matches its Crossref record; 9 of the 9 references it cites were found in a registry or an index.
The effect of mineral bond strength and adsorbed water on fault gouge frictional strength
Abstract
Recent studies suggest that the tendency of many fault gouge minerals to take on adsorbed or interlayer water may strongly influence their frictional strength. To test this hypothesis, triaxial sliding experiments were conducted on 15 different single‐mineral gouges with various water‐adsorbing affinities. Vacuum dried samples were sheared at 100 MPa, then saturated with water and sheared farther to compare dry and wet strengths. The coefficients of friction, μ, for the dry sheet‐structure minerals (0.2–0.8), were related to mineral bond strength, and dropped 20–60% with the addition of water. For non‐adsorbing minerals (μ = 0.6–0.8), the strength remained unchanged after saturation. These results confirm that the ability of minerals to adsorb various amounts of water is related to their relative frictional strengths, and may explain the anomalously low strength of certain natural fault gouges.
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Citations
Cites
Byerlee, J. (1978) · pure and applied geophysics · doi:10.1007/bf00876528 · Cited by 4,029
Heat flow and energetics of the San Andreas Fault Zone
Lachenbruch, A. H., & Sass, J. H. (1980) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb085ib11p06185 · Cited by 868
Dynamic Properties of Molecularly Thin Liquid Films
Israelachvili, J. N., McGuiggan, P. M., & Homola, A. M. (1988) · Science · doi:10.1126/science.240.4849.189 · Cited by 664 · cited 1×
“Israelachvili et al. (1988) demonstrated that for mineral grains that are separated by a thin film of water, the first few layers of water are organized at an atomic level and the shear strength i s inversely related to the number of water layers present.”
BackgroundPore pressure diffusion and the mechanism of reservoir-induced seismicity
Talwani, P., & Acree, S. (1984) · Pure and Applied Geophysics · doi:10.1007/bf00876395 · Cited by 366
Strengths of serpentinite gouges at elevated temperatures
Moore, D. E., Lockner, D. A., Ma, S., Summers, R., & Byerlee, J. D. (1997) · Journal of Geophysical Research: Solid Earth · doi:10.1029/97jb00995 · Cited by 236
Self-citationEffect of humidity on time‐ and velocity‐dependent friction in rocks
Dieterich, J. H., & Conrad, G. (1984) · Journal of Geophysical Research: Solid Earth · doi:10.1029/jb089ib06p04196 · Cited by 231
Chapter 3 Frictional Strength and the Effective Pressure Law of Montmorillonite and lllite Clays
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Self-citationSymposium probes materials science approaches in geophysics
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The Mechanics of Earthquakes and Faulting
Scholz, C. H. (2019) · Cambridge University Press eBooks · doi:10.1017/9781316681473 · Cited by 910
Saffer, D. M., & Marone, C. (2003) · Earth and Planetary Science Letters · doi:10.1016/s0012-821x(03)00424-2 · Cited by 586
On the relation between fault strength and frictional stability
Ikari, M. J., Marone, C., & Saffer, D. M. (2011) · Geology · doi:10.1130/g31416.1 · Cited by 379
Bos, B., & Spiers, C. J. (2002) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2001jb000301 · Cited by 306
Tectonic significance of serpentinites
Guillot, S., Schwartz, S., Reynard, B., Agard, P., & Prigent, C. (2015) · Tectonophysics · doi:10.1016/j.tecto.2015.01.020 · Cited by 275
Metadata
- Authors
- Morrow, C. A., Moore, D. E., & Lockner, D. A.
- Venue
- Geophysical Research Letters
- Publisher
- American Geophysical Union (AGU)
- Published
- 2000-03-15
- Volume
- 27
- Issue
- 6
- Pages
- 815-818
- ISSN
- 0094-8276 (ISSN-L)
- 1944-8007
- OpenAlex
- W2072676217
- Cited by
- 386
- References
- 9
- FWCI
- 2.81
- Type
- journal article
- Language
- en
- Open access
- closed
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- Morrow, C. A., Moore, D. E., & Lockner, D. A. (2000). The effect of mineral bond strength and adsorbed water on fault gouge frictional strength. Geophysical Research Letters. https://doi.org/10.1029/1999gl008401
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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).
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