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- W1001019692 abstract "Cla^7 minerals are found to be a significant component of all the fault zor^s, younn or old, at surface or at depth down to 2 k i ] o m e t e r s . These clays are stable up to 200 to 400 degrees under ] 4 kb of confining pressure. Thus, there are reasons to believe that in the part of the fault zone < h i c h earthquakes are found to occur we nav encounter clay goiuge. ^ e c b i c a 1 1 y , the clays are auite weak c o ni pared either to rocks or to frictional contacts of rocks. The peak strength under 2-4 kb confining pressure of montmori1Ionite, a common crouae mineral, is 0.25 to 0.35 kb; its residual strength is 1020% lower." @default.
- W1001019692 created "2016-06-24" @default.
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- W1001019692 date "1981-01-01" @default.
- W1001019692 modified "2023-09-26" @default.
- W1001019692 title "Rock mechanical investigation of clay and clayey gouge at high pressure and temperature" @default.
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- W1001019692 doi "https://doi.org/10.3133/ofr8194" @default.
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