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Stress sensitivity of fault seismicity: a comparison between limited-offset oblique and major strike-slip faults... We can explain the different behavior of the two styles of faults if those with large cumulative offset become impermeable through gouge buildup; coseismically pressurized pore fluids could be trapped and negate imposed normal stress changes, whereas in more limited offset faults, fluids could rapidly escape....

général - core.ac.uk - PDF: walrus.wr.usgs.gov

Imbricate thrust stack model for the formation of glaciotectonic rafts : an example from the middle pleistocene of north norfolk, uk... Mechanisms for the detachment, transport and accretion of the rafts are explored, and it is concluded that pressurized pore water played an important role in all three phases....

PDF: nora.nerc.ac.uk