Time- and Temperature-Dependence of the Fluid Transport Properties, Strength and Mechanical Behaviour of Crustal Faults - An Experimental and Modelling Study

High temperature rock deformation experiments will be performed in conjunction with high resolution, computer-aided x-ray microtomography to determine time-dependent and temperature-dependent effects on fluid transport properties, strength and mechanical behaviour during slip and interseismic healing of simulated fault rocks in hydrothermal environments. The results will be used with cellular automaton modelling approaches to develop a quantitative understanding of how coupling between fluid flow and rock deformation controls earthquake rupture and fluid migration in fault networks in the continental seismogenic regime. This work will provide new understanding of triggers for earthquake nucleation and controls on localisation of ore deposits.