P M Fulton

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The frictional resistance on a fault during slip controls earthquake dynamics. Friction dissipates heat during an earthquake; therefore, the fault temperature after an earthquake provides insight into the level of friction. The Japan Trench Fast Drilling Project (Integrated Ocean Drilling Program Expedition 343 and 343T) installed a borehole temperature(More)
  • Patrick M Fulton, Gina Schmalzle, Robert N Harris, Timothy Dixon, P M Fulton
  • 2010
a r t i c l e i n f o The Carrizo segment of the San Andreas Fault separates rocks of the Salinian Block southwest of the fault characterized by high heat flow (~75–95 mW/m 2) and shallow seismicity (b~10 km depth), from rocks of the Franciscan Complex and Great Valley Group northeast of the fault associated with low heat flow (50–60 mW/m 2) and deeper(More)
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