Monitoring increases in fracture connectivity during hydraulic stimulations from temporal variations in shear-wave splitting polarization

Alan F. Baird, J.-Michael Kendall, James P. Verdon, Andreas Wuestefeld, Todd E. Noble, Yongyi Li, Martin Dutko, and Quentin J. Fisher
Geophysical Journal International 195 (2), 1120–1131.

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Abstract: Hydraulic overpressure can induce fractures and increase permeability in a range of geologic settings including volcanological, glacial, and petroleum reservoirs. Here we consider an example of induced hydraulic fracture stimulation in a tight gas sandstone. Successful exploitation of tight-gas reservoirs requires fracture networks, either naturally occurring, or generated through hydraulic stimulation. The study of seismic anisotropy provides a means to infer properties of fracture networks, such as the dominant orientation of fracture sets and fracture compliances. Shear-wave splitting from microseismic data acquired during hydraulic fracture stimulation allows us to not only estimate anisotropy and fracture properties, but also to monitor their evolution through time. Here we analyse shear-wave splitting using microseismic events recorded during a multi-stage hydraulic fracture stimulation in a tight gas sandstone reservoir. A substantial rotation in the dominant fast polarization direction (ψ) is observed between the events of stage 1 and those from later stages. Although large changes in ψ have often been linked to stress-induced changes in crack orientation, here we argue that it can better be explained by a smaller fracture rotation coupled with an increase in the ratio of normal to tangential compliance (ZN/ZT) from 0.3 to 0.6. ZN/ZT is sensitive to elements of the internal architecture of the fracture, as well as fracture connectivity and permeability. Thus, monitoring ZN/ZT with shear-wave splitting can potentially allow us to remotely detect changes in permeability caused by hydraulic stimulation in a range of geologic settings.