2012
DOI: 10.1130/b30753.1
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Fault kinematics and surface deformation across a releasing bend during the 2010 MW 7.1 Darfield, New Zealand, earthquake revealed by differential LiDAR and cadastral surveying

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Cited by 55 publications
(63 citation statements)
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“…The data were collected a few days after the earthquake and were used along with a variety of other data to measure the surface displacement resulting from the earthquake and to interpret the kinematics of the Greendale Fault (Duffy et al, 2012).…”
Section: Case Studiesmentioning
confidence: 99%
“…The data were collected a few days after the earthquake and were used along with a variety of other data to measure the surface displacement resulting from the earthquake and to interpret the kinematics of the Greendale Fault (Duffy et al, 2012).…”
Section: Case Studiesmentioning
confidence: 99%
“…Multi-source, multi-period DTM data are not only a critical tool for research on the mechanism of landslides, but also considered as greatly useful information regarding active faults, earthquake disasters [1][2][3][4], and flooding/river bank erosion [5]. When it comes to the comparison of this type of terrain information, error estimation of data obtained in various periods using various techniques becomes crucial.…”
Section: Introductionmentioning
confidence: 99%
“…To work with LiDAR point clouds directly, Nissen et al [46] introduced a new method for calculating 3-D coseismic surface displacements from preand post-earthquake LiDAR data based on the Iterative Closest Point (ICP) algorithm [52,53]. The method was also used to extract threedimensional displacements and rotations from pre-and postearthquake LiDAR data for the 2008 Iwate-Miyagi earthquake and the 2011 Fukushima-Hamadori earthquake in Japan [49]. One limitation of the method by Nissen et al [46,49] is that it is based on the assumption that all LiDAR points in the compared point clouds have uniform accuracy, whereas the error for each LiDAR point depends on variable factors such as the range from system to target and the incidence angle of laser beam.…”
Section: Surface Deformation Revealed By Differential Lidarmentioning
confidence: 99%
“…The method was also used to extract threedimensional displacements and rotations from pre-and postearthquake LiDAR data for the 2008 Iwate-Miyagi earthquake and the 2011 Fukushima-Hamadori earthquake in Japan [49]. One limitation of the method by Nissen et al [46,49] is that it is based on the assumption that all LiDAR points in the compared point clouds have uniform accuracy, whereas the error for each LiDAR point depends on variable factors such as the range from system to target and the incidence angle of laser beam. To take into account the random errors in differential LiDAR point clouds, Zhang et al [47] developed an error propagation method to generate an estimated random error for each LiDAR point, and obtain 3D displacements between two LiDAR point clouds using an anisotropic weighted ICP algorithm.…”
Section: Surface Deformation Revealed By Differential Lidarmentioning
confidence: 99%
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