WebAug 20, 2014 · Fluid-rock reaction weakening of fault zones Journal Article Wintsch, R ; Christoffersen, R ; Kronenberg, A - Journal of Geophysical Research The presence of … WebApr 8, 2024 · Key Points At low temperature and pressure, chlorite is weak and velocity-strengthening and hornblende and epidote are strong and velocity-weakening Increasing chlorite content leads to mixtures becoming frictionally weaker and velocity-strengthening
Fluid-rock Reaction Weakening of Fault Zones
WebThe low permeabilities measured support models invoking high fluid pressure weakening of large faults with minimal fluid loss. The stability of structured water films with varying temperature, water pressure and water chemistry may produce a heterogeneous permeability profile with depth in fault zones. WebDec 1, 2024 · The growth of phyllosilicates is favored in meteoric water-dominated granitic fault systems, where mineral-aqueous fluid equilibria predict that modal phyllosilicate will … desk and chair on clearance
Evolution of strength recovery and permeability during …
WebAug 10, 2024 · Extensive fluid–rock reaction can produce layers of phyllosilicates, which can significantly weaken fault zones, as discussed below (e.g. Wintsch et al. 1995; Imber et al. 1997). A second difficulty in applying Byerlee's Law to the Earth relates to the composition of fault rocks. WebNov 15, 2011 · Here, we show that fault zone structure has an important influence on mixed-mode fault slip behavior. Our field studies depict a complex fault zone structure where foliated horizons surround meter- to decameter-sized lenses of competent material. The foliated rocks are composed of weak mineral phases, possess low frictional … WebJul 10, 1995 · Abstract. The presence of weak phyllosilicates may explain the low shear strengths of fault zones if they define well-developed fabrics. The growth of … desk and chair rental