Search

To understand the geomechanical implications of long-term creep (time-dependent deformation) response of gas shale, short-duration creep was recorded from laboratory triaxial tests on ten Goldwyer gas shale samples in the onshore Canning Basin at in situ stress conditions under constant differential axial stress. A simple power-law function captures primary creep behaviour involving elastic compliance constant B and time-dependent factor n. Experimental creep data revealed larger axial creep strain in clay and organic-rich rocks, than those dominated by carbonates. Anisotropic nature of creep was observed depending upon the direction of constant axial stress application (perpendicular or parallel to the bedding plane). Upon the application of linear viscoelastic theory on laboratory creep fitting coefficients, differential horizontal stress accumulation over a geological time scale was estimated from the viscoelastic stress relaxation concept. Further, this model was used to derive lithology-dependent least principal stress (Shmin) magnitude at depth for two vertical wells intersecting the Goldwyer gas shale formations. This newly proposed Shmin model was found to have a profound influence on designing hydraulic fracture simulation. Further, pore size distribution and specific surface area value SN2 were derived from low-pressure gas adsorption experiments. These physical properties along with weak mineral components were linked with creep constitutive parameters to understand the physical mechanisms of creep. A strong correlation was noted between SN2 and creep parameters n and B. Finally, an attempt was made to investigate how gas shale composition and failure frictional properties can influence shear fracturing. Highlights: Bedding perpendicular gas shales show a higher creep magnitude than their bedding parallel orientation i.e., creep deformation is anisotropic in nature. A viscoelastic stress relaxation approach can explain lithology-dependent least principal stress Shmin profile estimated from 1-D power-law creep constitutive parameters (B—elastic compliance constant, n—time-dependent factor) and with a constrain of relative variation of in situ stress magnitudes ϕ at subsurface depth. Specific surface area SN2 is a first-order proxy for continuous creep constitutive parameters prediction as well as estimation of frictional failure properties of gas shales intersecting different stratigraphic layers. [ABSTRACT FROM AUTHOR]