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Abstract

There is mounting evidence that the fluid-saturated stress-aligned intergranular microcracks present in almost all rocks are geometrically close to the critical state where small-scale changes may have significant large-scale effects even at considerable distances.

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/content/papers/10.3997/2214-4609.201408555
1998-06-08
2024-04-26
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.201408555
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