FRACTURING AND HYDROTHERMAL ALTERATION IN NORMAL-FAULT ZONES

Large normal fault zones are characterized by intense fracturing and hydrothermal alteration. Displacement is localized in a slip zone of cataclasite, breccia and phyllonite surrounding corrugated and striated fault surfaces. Slip zone rock grades into fractured, but less comminuted and hydrothermally altered rock in the transition zone, which in turn grades abruptly into the wall rock. Fracturing and fluid flow is episodic, because permeability generated during earthquakes is destroyed by hydrothermal processes during the time between earthquakes. Fracture networks are described by a fracture fabric tensor (F). The permeability tensor (k) is used to estimate fluid transport properties if the trace of F is sufficiently large. Variations in elastic moduli and seismic velocities between fault zone and wall rock are estimated as a function of fracture density (epsilon). Fracturing decreases elastic moduli in the transition zone by 50 100% relative to the country rock, and similar or even greater changes presumably occur in the slip zone. P- and S-wave velocity decrease, and V(p)/V(s) increases in the fault zone relative to the wall rock. Fracture permeability is highly variable, ranging between 10(-13) m2 and 10(-19) m2 at depths near 10 km. Changes in permeability arise from variations in effective stress and fracture sealing and healing. Hydrothermal alteration of quartzo-feldspathic rock at T > 300-degrees-C creates mica, chlorite, epidote and alters the quartz content. Alteration changes elastic moduli, but the changes are much less than those caused by fracturing. P- and S-wave velocities also decrease in the hydrothermally altered fault rock relative to the country rock, and there is a slight decrease in V(p)/V(s), which partially offsets the increase in V(p)/V(s) caused by fracturing. Fracturing and hydrothermal alteration affect fault mechanics. Low modulus rock surrounding fault surfaces increases the probability of exceeding the critical slip distance required for the onset of unstable slip during rupture initiation. Boundaries between low modulus fault rock and higher modulus wall rock also act as rupture guides and enhance rupture acceleration to dynamic velocity. Hydrothermal alteration at temperatures in excess of 300-degrees-C weakens the deeper parts of the fault zone by producing-phyllitic mineral assemblages. Sealing of fracture in time periods between large earthquakes generates pods of abnormally pressured fluid which may play a fundamental role in the initiation of large earthquakes.