Fluid-rock reaction weakening of fault zones
WebJul 10, 1995 · Fluid-rock Reaction Weakening of Fault Zones July 1995 DOI: Authors: Robert P. Wintsch Indiana University Bloomington R. Christoffersen AK Kronenberg … 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 …
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 …
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 …
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... 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 …
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 …
WebFeb 4, 2010 · 1. Introduction [2] The apparent weakness of mature faults with large offsets (>5 km) and the state of stress in the Earth's crust have long been a matter of debate. … north korean writing systemWebFeb 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 ]. how to say married in frenchWebwhere c is the concentration of an element in rock or fluid (mass%). The initial δ rock 0 value can be obtained by the analysis of fresh, unaltered rock, whereas the final δ rock … how to say marleneWebJan 30, 2003 · The experimental results show how hydrothermal reactions in fault zones may lead to two competing, time-dependent effects; fault strengthening due to increased … how to say mark in japaneseWebDec 17, 2009 · We show that fault weakening depends strongly on rock fabric and the distribution of weak phases within a fault zone. how to say mark in frenchWebThe 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. north korea of central asiaWebAug 1, 2014 · Fault rocks contain graphite veins and cement that locally constitute >50% of the rock. Individual graphite veins are as much as 1 cm wide, and are locally almost pure graphite, with minor muscovite and anatase. Hydrothermal graphite grain size (10–500 µm) is substantially greater than background metamorphosed organic matter (∼1 µm). north korea of europe