Difference between revisions of "Dictionary:Microcracks"

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A theory to explain the effect of pressure on the velocity of non-porous rocks. Minute cracks develop upon cooling because of differences between thermal expansion characteristics among the minerals of which the rock is composed. See Gardner et al. (1974).
 
A theory to explain the effect of pressure on the velocity of non-porous rocks. Minute cracks develop upon cooling because of differences between thermal expansion characteristics among the minerals of which the rock is composed. See Gardner et al. (1974).
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Latest revision as of 02:28, 16 April 2019

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A theory to explain the effect of pressure on the velocity of non-porous rocks. Minute cracks develop upon cooling because of differences between thermal expansion characteristics among the minerals of which the rock is composed. See Gardner et al. (1974).