1887

Abstract

The deformation of high porosity chalks has become a major factor in understanding their performance as<br>hydrocarbon reservoirs. Chalks with porosities in excess of 30% readily undergo large volumetric strains when<br>subject to fluid production and pore pressure depletion in many cases passing through a phase transition from<br>elastic to ductile compaction behaviour with commensurate large increases in compressibility.

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/content/papers/10.3997/2214-4609.201407547
1994-09-09
2020-10-26
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