Fluid-rock reaction weakening of fault zones
WebDec 1, 2024 · 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 equilibria predict that modal phyllosilicate will increase via feldspar replacement reactions. In … Webthrough a process of reaction weakening. Fluid-rock ... [1993] suggest that fluids penetrated the studied ancient fault zones throughout th• slip history and opisodic flow may
Fluid-rock reaction weakening of fault zones
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Webabstract. 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 … Webthis 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 ...
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 … WebDec 1, 2004 · Fluid‐rock reaction weakening of fault zones R. Wintsch, R. Christoffersen, A. Kronenberg Geology 1995 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… Expand 402 View 2 excerpts, …
WebMetamorphic core complexes and associated detachment faults of the North American Cordillera represent gently dipping, normal-displacement shear zones (detachment zones) along which hot, deeper levels of the crust were transported upward and outward from underneath a brittlely distended upper plate. Structures that formed during the ductile-to … WebAug 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).
WebMay 15, 2000 · The Great Glen Fault Zone (GGFZ) is a major, reactivated strike‐slip fault within the lower Paleozoic Caledonian orogenic belt of the British Isles. The Late Devonian to Tertiary reactivation history… Expand 60 PDF Save Alert Low effective fault strength due to frictional-viscous flow in phyllonites, Karakoram Fault Zone, NW India
WebJan 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 … portland sales taxportland rufcWebLarge normal fault zones are characterized by intense fracturing and hydrothermal alteration. Displacement is localized in a slip zone of cataclasite, breccia and phyllonite … portland schooner co. 1912WebFeb 1, 2004 · Several studies have focused on fluid-assisted reaction softening and fault weakening during the longterm evolution of fault zones (Caine et al., 1996; Holdsworth, 2004; Collettini et... portland schedule boosterWebDec 1, 2005 · In both fault types, early cataclasis facilitates fluid influx into the active fault zone, leading to widespread alteration of the crushed material (reaction softening) and simultaneously... portland salsa and bachata congressWebThe 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. optimum re insurance company dallas txWebJan 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 … portland school apartments portland mi