1887

Abstract

Hydrofracturing is an inprobable process in basins. Instead, dilational, shear-related deformations are predicted under the conditions that can normally be achieved. Such dilational responses explain the observed pressure profiles and the outcrop-based observations.

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/content/papers/10.3997/2214-4609.20145405
2010-04-26
2021-01-23
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609.20145405
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