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Understanding how natural fractures at multiple scales respond to pore pressure changes is essential for interpreting microseismicity and predicting stimulation performance in unconventional reservoirs. This study integrates analytical modeling, surface-seismic–based fracture characterization, and microseismic analysis to investigate how dual-scale natural fractures—small-scale distributed fractures and large-scale discrete networks—control hydraulic-fracturing behavior in the Weiyuan shale gas reservoir, Sichuan Basin, China. Field-calibrated fracture constitutive models and slip- and dilation-tendency analyses are used to evaluate stress- and scale-dependent hydro-mechanical responses and associated deformation modes. Spatial microseismic clustering is quantified using Ripley’s K-function, and b-value analysis characterizes fracture activation mechanisms and their temporal evolution. Modeling results show that initial aperture is the primary geometric control on fracture stiffness and closure behavior. Small-scale fractures deform mainly through normal-stress–driven opening and closure, whereas large-scale fractures undergo shear dilation, enhancing permeability. Field observations confirm the reactivation of large-scale, unfavorably oriented fractures. Microseismic clustering patterns reflect the geometry, density, and deformation modes of pre-existing fractures, delineating the spatial extent of stimulated zones and the connectivity of induced fracture networks. Spatial variations in b-value distinguish shear reactivation of large-scale fractures from fluid-driven tensile propagation in small-scale fracture zones, while temporal trends capture evolving deformation mechanisms during stimulation. Together, these results demonstrate that fracture scale, density, and deformation mode exert primary control on hydro-mechanical behavior and microseismic response, providing a mechanistic framework for designing geomechanically informed stimulation strategies in naturally fractured shale reservoirs.
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Meng et al. (2026) studied this question.
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