Fault kinematics and surface deformation across a releasing bend during the 2010 MW 7 . 1 Darfi eld , New Zealand , earthquake revealed by differential LiDAR and cadastral surveying

@inproceedings{Duffy2013FaultKA,
  title={Fault kinematics and surface deformation across a releasing bend during the 2010 MW 7 . 1 Darfi eld , New Zealand , earthquake revealed by differential LiDAR and cadastral surveying},
  author={Brendan Duffy and Mark A. Quigley and David J A Barrell and Russ Van Dissen and Timothy Stahl and S{\'e}bastien Leprince and Craig R. McInnes and Eric L. Bilderback},
  year={2013}
}
Dextral slip at the western end of the east-west–striking Greendale fault during the 2010 MW 7.1 Darfi eld earthquake transferred onto a northwest-trending segment, across an apparent transtensional zone, here named the Waterford releasing bend. We used detailed surface mapping, differential analysis of preand postearthquake light detection and ranging (LiDAR), and property boundary (cadastral) resurveying to produce high-resolution (centimeter-scale) estimates of coseismic ground-surface… CONTINUE READING

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