Large-Scale Bedding Plane Slippage and Its Impact on Hydraulic Fracturing: Integrated Analysis from Field Observations in the Eagle Ford and Austin Chalk Formations

Abstract This study presents the first documented field evidence of large-scale bedding plane slippage (BPS) induced by hydraulic fracturing operations in the Eagle Ford and Austin Chalk formations of southwest Texas. Using an integrated geophysical monitoring approach—including low-frequency Distributed Acoustic Sensing (LFDAS), surface-based microseismic monitoring, and time-lapse Vertical Seismic Profiling (VSP)—we investigate the complex fracture dynamics and fluid migration pathways resulting from stimulation. LFDAS measurements reveal migrating dipole strain signals consistent with shear-mode fractures propagating parallel to the monitor well, interpreted as BPS events. Microseismic moment tensor analyses support this interpretation, identifying horizontal-slip events concentrated near the treatment and monitor wells. Additionally, time-lapse VSP data indicates the reactivation of pre-existing vertical fractures, correlating with BPS signals and suggesting fluid communication between bedding planes and natural fracture networks. Geomechanical modeling using the three-dimensional Displacement Discontinuity Method (3D DDM) further validates that shear fractures along bedding planes can replicate observed LFDAS responses. These interactions between bedding planes and vertical fractures contribute to a more complex fracture network than anticipated, potentially enhancing reservoir connectivity and production performance. However, the findings also highlight potential inefficiencies and risks, including stage isolation due to conductive bedding plane and casing deformation due to shear displacement. This study underscores the need for adaptive completion design and well placement that account for natural fracture systems and bedding plane dynamics to optimize hydraulic fracturing efficiency and economic returns in similar unconventional reservoirs.