19 Faults, Fractures, and Geomechanics for the Energy Transition

This session explores the critical role of structural geology and geomechanics in the energy transition, emphasizing multidisciplinary research on faults, fractures, and deformation processes to ensure sustainable and efficient management of subsurface resources.

Sunday, 19 October 2025
8:00 AM - 12:00 PM
HBGCC, 302C


Pore Pressure-Stress Coupling Controls on Fault Reactivation and Fracture Evolution: Insights from Analytical Modeling and Case Studies

Paper number: 19-3
Program: Technical Sessions
Time: 8:45 AM – 9:00 AM


Authors

  • Dong Yang Presenting Author
    China University of Petroleum, Qingdao, 中国
  • Shang Xu
    China University of Petroleum, Qingdao, 中国
  • Bingchang Liu
    China University of Petroleum, Qingdao, 中国

Abstract

Pore pressure-stress coupling (PSC) governs stress redistribution during fluid injection and depletion in subsurface reservoirs, with significant implications for fault stability and fracture development. This study presents a quantitative analytical framework to assess how PSC influences fault slip tendency and fracture mode transitions across typical stress regimes. Closed-form expressions linking PSC magnitude to both slip tendency and critical pore pressure thresholds were derived and validated using a case study from the Dunkirk Shale in the Appalachian Basin. Results show that the effect of PSC on fault slip is directionally dependent: vertical PSC promotes fault reactivation in normal regimes but suppresses it in reverse regimes, while horizontal PSC exhibits the opposite behavior. Additionally, PSC raises the critical pressure required for fault reactivation, enhancing fault sealing capacity under certain conditions.

Fracture evolution is likewise sensitive to PSC magnitude. When PSC < 0.4, high differential stress promotes shear fractures; PSC > 0.4 favors tensile and hybrid fractures, with associated shifts in fracture orientation from vertical to bedding-parallel. These findings help explain the occurrence of horizontal microcracks and fibrous veins in overpressured mudrocks, and offer predictive insight into fracture network geometry under evolving pore pressure. This work highlights PSC as a key control on geomechanical behavior in reservoirs targeted for hydrocarbon production, CO₂ storage, and geothermal development, and underscores its role in supporting risk assessment and optimization efforts during the energy transition.


Geological Society of America Abstracts with Programs. Vol. 57, No. 6

doi: 10.1130/abs/2025AM-412081

© Copyright 2025 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.