The effect of temperature, the nature of the pore fluid, and subyield differential stress on the permeability of phyllosilicate-rich fault gouge

Elevated temperatures and subyield deviatoric stresses were applied to oriented natural samples of clay‐bearing fault gouge under pressure in order to establish their effects on the water and argon permeability under conditions closer to those found at depth in fault zones. It was found that the app...

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Veröffentlicht in:Journal of Geophysical Research - Solid Earth 2003-05, Vol.108 (B5), p.2227-n/a
Hauptverfasser: Faulkner, D. R., Rutter, E. H.
Format: Artikel
Sprache:eng
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