Laboratory results indicating complex and potentially unstable frictional behavior of smectite clay

Author:

Saffer Demian M.,Frye Kevin M.,Marone Chris,Mair Karen

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference22 articles.

1. Hydration-phase diagrams and friction of montmorillonite under laboratory and geologic conditions, with implications for shale compaction, slope stability, and strength of fault gouge;Bird;Tectonophysics,1984

2. Heat flow and stress along the San Andreas fault near Hollister, California;Brune;Geol. Soc. Am. Special Paper,1969

3. Composite planar fabric of fault gouge from the Punchbowl Fault, California;Chester;J. Struct. Geol.,1987

4. Role of pressure in smectite dehydration: effects on geopressures and smectite-to-illite transformation;Colten-Bradley;Am. Assoc. Pet. Geol. Bull,1987

5. Stress-induced smectite dehydration: ramifications for patterns of freshening and fluid expulsion in the N. Barbados accretionary wedge;Fitts;Eart. Planet. Sci. Lett.,1999

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