A new theory for the static contact between rough, unmated surfaces in non-elastically deforming rock and its implications for rock friction
- 31 December 1989
- journal article
- Published by Elsevier in Journal of Structural Geology
- Vol. 11 (7) , 787-798
- https://doi.org/10.1016/0191-8141(89)90098-9
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Growth of contact area between rough surfaces under normal stressGeophysical Research Letters, 1987
- Electrical conductivity of brine‐saturated fractured rockGeophysics, 1986
- closure of rock jointsJournal of Geophysical Research, 1986
- The effect of normal stress on the real area of contact during frictional sliding in rocksPure and Applied Geophysics, 1986
- Rock surface roughness and frictional strengthInternational Journal of Rock Mechanics and Mining Sciences, 1985
- Compressional and shear velocities of dry and saturated jointed rock: a laboratory studyGeophysical Journal International, 1985
- Closure of random elastic surfaces in contactJournal of Geophysical Research, 1985
- A new model for analyzing the effect of fractures on compressibilityJournal of Geophysical Research, 1979
- Friction of rocksPure and Applied Geophysics, 1978
- Behavior of rock salt, limestone, and anhydrite during indentationJournal of Geophysical Research, 1960