Slip rate on the San Diego trough fault zone, inner California Borderland, and the 1986 Oceanside earthquake swarm revisited

@article{Ryan2012SlipRO,
  title={Slip rate on the San Diego trough fault zone, inner California Borderland, and the 1986 Oceanside earthquake swarm revisited},
  author={H. Ryan and J. Conrad and C. Paull and M. McGann},
  journal={Bulletin of the Seismological Society of America},
  year={2012},
  volume={102},
  pages={2300-2312}
}
The San Diego trough fault zone (SDTFZ) is part of a 90-km-wide zone of faults within the inner California Borderland that accommodates motion between the Pacific and North American plates. Along with most faults offshore southern California, the slip rate and paleoseismic history of the SDTFZ are unknown. We pre- sent new seismic reflection data that show that the fault zone steps across a 5-km-wide stepover to continue for an additional 60 km north of its previously mapped extent. The 1986… Expand
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