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Title: Geophysical and Mineralogical Controls on the Rheology of Fracture Slip and Seal Breaching (Final Report)

Technical Report ·
DOI:https://doi.org/10.2172/1487035· OSTI ID:1487035
 [1];  [2];  [2];  [1];  [1];  [1];  [2];  [1]
  1. Pennsylvania State Univ., University Park, PA (United States)
  2. Princeton Univ., NJ (United States)

This work explores the geophysical and mineralogical controls on the rheology of fractures and faults to define the modes of permeability evolution and the potential for the breaching of seals for subsurface reservoirs. In particular, the work is arranged to determine the dynamic response of faults to shear reactivation (Parts I-III), their post slip and inter-seismic healing (Parts IV-V), their response to chemically reactive alteration (Parts VI-VII) and then upscaling via digital rock physics models (Parts IIX-XI). The work first defines the principal controls on frictional strength and stability in caprocks and unconventional reservoirs and their consequences for permeability evolution in shales (Part I). This linkage is extended to explore the impact of both mineralogy (Part II) and fracture roughness (Part III) on permeability evolution and to link this to the frictional and stability behavior of faults. The important impacts of post-slip healing during interseismic periods is then delineated (Part IV) and constrained using tightly controlled observations of reactivation displacements and permeability measurement (Part V). The role of corrosive fluids in both dissolving (Part VI) and transforming (Part VII) minerals within the fracture walls and cements is then explored, together with impacts on friction, stability and permeability. Finally, process-based models are applied to upscale the friction-stability-permeability response of both gouge-filled faults (Parts VIII and IX) and rough fractures (Part X) together with chemically-driven compaction impacting long-term interseismic sealing (Part XI).

Research Organization:
Pennsylvania State Univ., University Park, PA (United States)
Sponsoring Organization:
USDOE Office of Fossil Energy and Carbon Management (FECM)
DOE Contract Number:
FE0023354
OSTI ID:
1487035
Report Number(s):
Project-DE-FE0023354
Country of Publication:
United States
Language:
English

References (10)

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Understanding induced seismicity journal December 2016
The influence of Preslip Sealing on the Permeability Evolution of Fractures and Faults journal January 2018
The transition from steady frictional sliding to inertia-dominated instability with rate and state friction journal January 2019
Mineralogical Controls on Frictional Strength, Stability, and Shear Permeability Evolution of Fractures journal May 2018
Influence of weakening minerals on ensemble strength and slip stability of faults: Influence of Weakening Minerals on Fault journal September 2017
Frictional stability-permeability relationships for fractures in shales: Friction-Permeability Relationships journal March 2017
Seismicity-permeability coupling in the behavior of gas shales, CO2 storage and deep geothermal energy journal January 2017
Influence of Rock Mineralogy on Reactive Fracture Evolution in Carbonate-Rich Caprocks journal August 2018
Surface characteristics and permeability enhancement of shale fractures due to water and supercritical carbon dioxide fracturing journal June 2018