Rock Physics of Shale - Stanford University
Rock Physics of Shale - Stanford University
Rock Physics of Shale - Stanford University
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Brittleness: Examples<br />
Low Clay (tight sandstone) High Clay Fraction<br />
Porosity .01<br />
Clay .12<br />
Porosity .05<br />
Clay .31<br />
Porosity .05<br />
Clay .63<br />
In these examples, ductility depends on (1) composition and (2)<br />
confining stress.<br />
Brittle failure has little or no plastic flow before failure.<br />
Jizba, 1991, Ph.D. Dissertation, <strong>Stanford</strong> <strong>University</strong>.<br />
Jizba, 1991, Ph.D.<br />
dissertation, <strong>Stanford</strong><br />
Univ.<br />
53<br />
Gary Mavko – <strong>Stanford</strong> <strong>Rock</strong> <strong>Physics</strong> Laboratory