Show source-provided references
3. Laboratory Investigation of the Shear Failure Process and Strength Characteristics of a Rock Mass Containing Discontinuous Joints under Water Pressure Influence
10.1007/s10064-021-02565-z ↗15. Decrypting Healed Fault Zones: How Gouge Production Reduces the Influence of Fault Roughness
10.1093/gji/ggab003 ↗17. A Comparison of Seismicity Characteristics and Fault Structure Between Stick–Slip Experiments and Nature
10.1007/s00024-013-0713-7 ↗22. Additional Shear Resistance from Fault Roughness and Stress Levels on Geometrically Complex Faults
10.1002/jgrb.50262 ↗27. “Lab-Quakes”: Quantifying the Complete Energy Budget of High-Pressure Laboratory Failure
10.1029/2025AV001683 ↗30. Ulusay, R. (2015). The Present and Future of Rock Testing: Highlighting the ISRM Suggested Methods. The ISRM Suggested Methods for Rock Characterization, Testing and Monitoring: 2007–2014, Springer International Publishing.
10.1007/978-3-319-07713-0 ↗31. Cyclic Water Injection Potentially Mitigates Seismic Risks by Promoting Slow and Stable Slip of a Natural Fracture in Granite
10.1007/s00603-021-02438-7 ↗36. What Allows Seismic Events to Grow Big? Insights from b-Value and Fault Roughness Analysis in Laboratory Stick-Slip Experiments
10.1130/G39147.1 ↗37. Frictional Sliding Behaviour of Rough Fracture in Granite Under True Triaxial Loading with Implications for Fault Reactivation
10.1007/s00603-023-03561-3 ↗39. Fracture Mechanics Determine the Lengths of Interface Ruptures That Mediate Frictional Motion
10.1038/nphys3539 ↗40. Laboratory Observations of Slow Earthquakes and the Spectrum of Tectonic Fault Slip Modes
10.1038/ncomms11104 ↗44. A Constitutive Scaling Law and a Unified Comprehension for Frictional Slip Failure, Shear Fracture of Intact Rock, and Earthquake Rupture
10.1029/2000JB000123 ↗50. Unloading-Induced Instability of a Simulated Granular Fault and Implications for Excavation-Induced Seismicity
10.1016/j.tust.2017.01.002 ↗51. Intermittent Criticality Multi-Scale Processes Leading to Large Slip Events on Rough Laboratory Faults
10.1029/2023JB028411 ↗52. The Effect of Shear Displacement and Wear on Fault Stability: Laboratory Constraints
10.1029/2022JB026191 ↗55. Permeability Evolution and Frictional Stability of Fabricated Fractures with Specified Roughness
10.1029/2018JB016215 ↗58. Karner, S.L., and Marone, C. (2000). Effects of Loading Rate and Normal Stress on Stress Drop and Stick-Slip Recurrence Interval. Geocomplexity and the Physics of Earthquakes, American Geophysical Union. Washington DC American Geophysical Union Geophysical Monograph Series.
10.1029/GM120p0187 ↗59. On the Mechanics of Granular Shear: The Effect of Normal Stress and Layer Thickness on Stick-Slip Properties
62. Evolution of Shear Fabric in Granular Fault Gouge from Stable Sliding to Stick Slip and Implications for Fault Slip Mode
63. Foreshock Activity Promoted by Locally Elevated Loading Rate on a 4-m-Long Laboratory Fault
10.1029/2021JB023336 ↗64. Observed Source Parameters for Dynamic Rupture with Non-Uniform Initial Stress and Relatively High Fracture Energy
10.1016/j.jsg.2011.11.013 ↗69. Geologic Carbon Storage Is Unlikely to Trigger Large Earthquakes and Reactivate Faults through Which CO2 Could Leak
10.1073/pnas.1413284112 ↗