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Creator:: Fulton, Patrick M., Harris, Robert N., Saffer, Demian M., and Brodsky, Emily E.
Abstract:: Knowledge of frictional resistance along faults is important for understanding the mechanics of earthquakes and faulting. The clearest in situ measure of fault friction potentially comes from temperature measurements in boreholes crossing fault zones within a few years of rupture. However, large temperature signals from frictional heating on faults have...
Resource Type:: Article
Full Text:: on faults after large earthquakes? Patrick M. Fulton,1 Robert N. Harris,1 Demian M. Saffer,2 and

Creator:: Fulton, Patrick M., Saffer, Demian M., Harris, Robert N., and Bekins, Barbara A.
Abstract:: Improved interpretations of the strength of the San Andreas Fault near Parkfield, CA based on thermal data require quantification of processes causing significant scatter and uncertainty in existing heat flow data. These effects include topographic refraction, heat advection by topographically-driven groundwater flow, and uncertainty in thermal conductivity. Here, we re-evaluate...
Resource Type:: Article
Full Text:: : Evidence for a weak San Andreas Fault Patrick M. Fulton,1 Demian M. Saffer,1 Robert N. Harris,2 and

Creator:: Ellis, Susan, Fagereng, Åke, Barker, Dan, Henrys, Stuart, Saffer, Demian, Wallace, Laura, Williams, Charles, and Harris, Rob
Abstract:: We estimate fluid sources around a subducted seamount along the northern Hikurangi subduction margin of New Zealand, using thermomechanical numerical modelling informed by wedge structure and porosities from multichannel seismic data. Calculated fluid sources are input into an independent fluid-flow model to explore the key controls on overpressure generation to...
Resource Type:: Article

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