Abstract
No abstract available. doi:10.2204/iodp.sd.s01.39.2007
Highlights
SAFOD is located in central California within the transition between the creeping and locked sections of the San Andreas Fault, 9 km NW of Parkfield, Ca li f . a n d j u s t N W o f t h e r u p t u r e zone of the 2004 M6.0 Parkfield earthquake
T h e U n i v e r s i t y o f C a l i f o r n i a - B e r k e l e y High Resolution Seismic Network h a s o b s e r v e d i n d i v i d u a l earthquakes to recur every few years at precisely the same location and with the same magnitude (Nadeau and McEvilly, 1997; Nadeau et al, 2004)
Repeating sources of up to M2 are located at depths as shallow as 3 km at the SAFOD site, and they p la y a k e y r o l e in g u id in g S A F O D d r il l in g
Summary
SAF 83o depth (Boness and Zoback, 2006). In addition, heat flow measurements in the SAFOD pilot hole and main hole (to 3.1 km depth) are consistent with shallower data in the region which show no evidence of frictionally-generated heat (Williams et al, 2004; 2006).
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