Effect of pore pressure magnitude on the frictional properties and permeability evolution of fractures in schist
Author:
Funder
U.S. Department of Energy
Publisher
Springer Science and Business Media LLC
Subject
Economic Geology,General Energy,Geophysics,Geotechnical Engineering and Engineering Geology
Link
https://link.springer.com/content/pdf/10.1007/s40948-022-00504-0.pdf
Reference42 articles.
1. Andrews DJ (2002) A fault constitutive relation accounting for thermal pressurization of pore fluid. J Geophys Res: Solid Earth 107(B12):ESE-15
2. Bao X, Eaton DW (2016) Fault activation by hydraulic fracturing in western Canada. Science 354(6318):1406–1409
3. Brace WF, Martin RJ (1968) A test of the law of effective stress for crystalline rocks of low porosity. Int J Rock Mech Mining Sci Geomech Abstr 5(5):415–426
4. Byerlee JD (1968) Brittle-ductile transition in rocks. J Geophys Res 73(14):4741–4750
5. Candela T et al (2015) Flow rate dictates permeability enhancement during fluid pressure oscillations in laboratory experiments. J Geophys Res: Solid Earth 120(4):2037–2055
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