Abstract
The Pajarito fault system is a complex zone of deformation and a seismically active region nestled within the Rio Grande rift in north-central New Mexico. Numerous laterally discontinuous faults and associated folds and fractures interact in a manner that has important implications for seismic hazards and risk mitigation. Previous efforts have established a foundation for the location of lineaments and structures in the Pajarito fault system; however, ensuring the completeness of the current lineament mapping is required for identifying areas for field validation, evaluating the potential for future seismic activity, and better understanding fault interaction. Assistance with this fault-mapping task via automated or semiautomated techniques as applied to lidar data over a large area of interest is highly desirable. A proof-of-concept processing flow which transforms lidar point-cloud data into a raster of surfi-cial fault candidates is described and illustrated herein. These initial results hold great promise toward achieving our ultimate goal.
| Original language | English |
|---|---|
| Pages (from-to) | 391-397 |
| Number of pages | 7 |
| Journal | Photogrammetric Engineering and Remote Sensing |
| Volume | 88 |
| Issue number | 6 |
| DOIs | |
| State | Published - Jun 2022 |
| Externally published | Yes |
Funding
This research was conducted as a part of the Los Alamos National Laboratory Seismic Hazards Program, which is supported by the Office of Nuclear Safety within Los Alamos National Laboratory’s Associate Laboratory Directorate for Facilities and Operations. This is Los Alamos National Laboratory publication LA-UR-21-28106.