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The effect of mineral bond strength and adsorbed water on fault gouge frictional strength

Morrow, C. A., Moore, D. E., Lockner, D. A.·2000·Geophysical Research Letters

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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Crossref · 10.1029/1999gl008401

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Metadata

Authors
Morrow, C. A., Moore, D. E., & Lockner, D. A.
Venue
Geophysical Research Letters
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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CoChat. (2026). Citation check: The effect of mineral bond strength and adsorbed water on fault gouge frictional strength. https://app.cochat.ai/papers/10.1029/1999gl008401
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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).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.