2015
DOI: 10.4172/2169-0049.1000136
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LiDAR Data for Characterizing Linear and Planar Geomorphic Markers in Tectonic Geomorphology

Abstract: This paper provides a brief review of airborne light detection and ranging (LiDAR) data for characterizing linear and planar geomorphic markers in tectonic geomorphology, including traces of active faults and surface deformation caused by earthquakes. Challenges and opportunities of LiDAR for the study of tectonic geomorphology and coseismic deformation are also discussed.

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Cited by 7 publications
(4 citation statements)
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“…Within the last 2 decades, the explosion in sub-meter resolution airborne LiDAR data raises the reliability and practicality of geomorphological mapping (Nissen et al, 2012;Lin et al, 2013;Dong, 2015). Compared with largescale DEM data mentioned above, DEMs derived from LiDAR are of great advantage with respect to the detailed description of microscopic topographic elements related to tectonic activities and surface processes.…”
Section: Automated Geomorphological Mappingmentioning
confidence: 99%
“…Within the last 2 decades, the explosion in sub-meter resolution airborne LiDAR data raises the reliability and practicality of geomorphological mapping (Nissen et al, 2012;Lin et al, 2013;Dong, 2015). Compared with largescale DEM data mentioned above, DEMs derived from LiDAR are of great advantage with respect to the detailed description of microscopic topographic elements related to tectonic activities and surface processes.…”
Section: Automated Geomorphological Mappingmentioning
confidence: 99%
“…and visual assessment of channel reconstruction. While lidar data are being increasingly used in tectonic geomorphology (Lin et al, 2009(Lin et al, , 2013Dong, 2015;Dong and Chen, 2018), few studies have been conducted for the analysis of channel longitudinal profiles derived from lidar data to support morphotectonic studies. This can be partly attributed to the following reasons: (1) Some lidar data for morphotectonic studies are usually acquired in a limited area along active faults and do not include complete drainage areas or channel heads, prohibiting the use of traditional methods for channel extraction; (2) geologists often need to select one major channel and obtain longitudinal profiles and measurements from the main channel efficiently (for example, Ouchi [2005] measured ten offset channels across the San Andreas fault by walking along each channel and taking measurements for analysis of channel development); yet a flexible and accurate tool is not available in current GIS software packages.…”
Section: Software Contributionmentioning
confidence: 99%
“…Light detection and ranging (lidar) has provided unprecedented details of Earth's surface features in the past two decades (Woolard and Colby, 2002;Staley et al, 2006;Arrowsmith and Zielke, 2009;Dong, 2012Dong, , 2015Dong and Chen, 2018). Many studies have been carried out specifically for channel analysis using lidar data (Cavalli et al, 2008;Passalacqua et al, 2010aPassalacqua et al, , 2010bHunt and Royall, 2013;Hooshyar et al, 2015).…”
Section: ■ Introductionmentioning
confidence: 99%
“…Light detection and ranging (lidar) can be used to identify submeter-scale geomorphic features (Dong, 2015). Currently, this is done by analyzing individual profiles across fault scarps, manually picking fault components on distance vs. elevation plots, calculating statistics and regressions for each, and then running unique analyses for each profile, which is both tedious and time-consuming.…”
Section: Introductionmentioning
confidence: 99%