Influence of normal stress and temperature on water content of (smectite) clays and possible implications for frictional strength of fault gouge
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- Type
- dissertation
- Published
- 2011-03-29
- Cited by
- 1
- References
- 85
- OpenAlex
- https://openalex.org/W174866771
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128167362
Keywords
Clay minerals, Geotechnical engineering, Stress (linguistics), Fault gouge, Normal fault
References
- The surface chemistry of soils
- Preliminary analysis of clay gouge from a well in the San Andreas fault zone in central California
- The Structure and Properties of Water
- Clay mineralogy : spectroscopic and chemical determinative methods
- Book Review: Experimental rock deformation. The Brittle Field. M.S. Paterson, Springer, Berlin-Heidelberg, 1978, 254 pp, DM 48.00, approx. US $ 24.00
- Experimental Rock Deformation: The Brittle Field
- Frictional properties of natural fault gouge from a low‐angle normal fault, Panamint Valley, California
- Crystal Structures of Clay Minerals and their X-ray Identification
- Cation Exchange Capacity of Kaolinite
- Swelling of clay minerals. A molecular simulation study
- The effect of F/OH substitution on some layer-silicate minerals
- Computer Simulation of Interlayer Molecular Structure in Sodium Montmorillonite Hydrates
- FTIR techniques in clay mineral studies
- Friction of rocks
- Constraints on mineralization, fluid-rock interaction, and mass transfer during faulting at 2―3 km depth from the SAFOD drill hole
- Stepwise Hydration of High-Quality Synthetic Smectite with Various Cations
- Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gouge
- Dehydration of Ca-montmorillonite at the crystal scale. Part I: Structure evolution
- Mechanical properties of clays at high pressure
- Clay swelling — A challenge in the oilfield
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