Fault Name |
State |
San Andres Mountains fault |
New Mexico |
Comments |
The preferred vertical slip rate is based on 6- to 15-m-high scarps that offset Picacho alluvium that is 70-130 ka (Machette, 1987). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Lund, W.R., ed., 2006, Basin and Range Province Earthquake Working Group seismic-hazard recommendations to the U.S. Geological Survey National Seismic Hazard Mapping Program: Utah Geological Survey Open-File Report 477, 23 p, ugspub.nr.utah.gov/publications/open_file_reports/OFR-477.pdf. Machette, M.N., 1987, Preliminary assessment of paleoseismicity at White Sands Missile Range, southern New Mexico—Evidence for recency of faulting, fault segmentation, and repeat intervals for major earthquakes in the region: U.S. Geological Survey Open-File Report 87-444, 46 p.
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