Fluid-rock reaction weakening of fault zones
WebSep 24, 2024 · Fault-zone fluids control effective normal stress and fault strength. While most earthquake models assume a fixed pore fluid pressure distribution, geologists have documented fault... 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
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WebJan 30, 2003 · The experiments presented here show that isostatic hydrothermal reaction of fault products formed in previously intact rock can result in significant strengthening of fault zones. Strength recovery of our experimental fault zones was achieved by compaction of gouge material and healing of crack arrays that were formed during initial … 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.
WebDec 17, 2009 · Explanations for fault weakness include the presence of weak minerals, high fluid pressures within the fault core and dynamic processes such as normal stress reduction, acoustic fluidization or extreme weakening at high slip velocity. WebMay 13, 2015 · Chemical reactions between the fluid and rock mass lead to erosion in the mineral particles and crystals, weakening of the particle bond strength, and changes in the mineral components...
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 phyllosilicates is favored in meteoric water-dominated granitic fault systems, where mineral-aqueous fluid … WebFluid-rock reaction weakening of fault zones. Wintsch, R. P. ; Christoffersen, R. ; Kronenberg, A. K. The presence of weak phyllosilicates may explain the low shear …
Webreaction weakening of fault zones In the absence of direct observations of high fluid pressure in active fault zones in crystalline rocks, the effects of fluids
WebJan 30, 2003 · The experiments presented here show that isostatic hydrothermal reaction of fault products formed in previously intact rock can result in significant strengthening of … green colored graniteWebFeb 4, 2010 · The degree of weakening depends on the thickness of the weak layer. In nature, talc and most other weak minerals (clays and phyllosilicates) are formed by chemical and hydration reactions [ Imber et al., 1997; Jefferies et al., 2006; Schleicher et al., 2006; Collettini et al., 2009b ]. flow sinus washWebMay 13, 2015 · We determine the evolution of frictional strength, strain weakening behavior and permeability in fractures subject to dissolution and precipitation. We establish these relations through slide–hold–slide experiments, with hold times from 10 to 3000 s, on split limestone core, under hydraulically open and closed conditions. Fracture friction and … green colored hanging ceiling lightsWebAug 20, 2014 · Fluid-rock reaction weakening of fault zones Journal Article Wintsch, R ; Christoffersen, R ; Kronenberg, A - Journal of Geophysical Research The presence of … green colored goldWebabstract. The presence of weak phyllosilicates may explain the low shear strengths of fault zones if they define well-developed fabrics. The growth of phyllosilicates is favored in … green colored hair sprayWebthis fault zone is weak in an absolute sense, although this remains a controversial issue. ... protolith (thereby allowing enhanced fluid-rock interaction) coupled with the development of a ... flows in the value chainWebJul 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 … flow sip and let go elizabeth nj