Earthquake fracture energy inferred from kinematic rupture models on extended faults

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Towards inferring earthquake patterns from geodetic observations of interseismic coupling (2010, background): “An approximation for Δ τ prop can be obtained by considering the difference in average shear stress on the patch before and during seismic slip and a further contribution from the breakdown wor”
A thermal pressurization model for the spontaneous dynamic rupture propagation on a three‐dimensional fault: 1. Methodological approach (2006, methodology): “This larger value does not follow the scaling law between d0 and L proposed in dry conditions by Bizzarri and Cocco [2003] because in that work they did not account for the effects of thermal pressurization caused by frictional heating.”
Inferring earthquake physics and chemistry using an integrated field and laboratory approach (2012, background): “Moreover, the value of the breakdownwork is on the low end (1e3 MJ/m2) compared to seismological estimates of large earthquakes worldwide (1e100 MJ/m2, e.g. Rice, 2006; Tinti et al., 2005).”
Heating and weakening of faults during earthquake slip (2006, background): “That is a feature shared by recent assemblies on data for large numbers of earthquakes [Abercrombie and Rice, 2005; Rice et al., 2005; Tinti et al., 2005], all of which show a clear tendency for the average G in an event, as inferred from seismic slip inversions, to increase with the average slip in”