Comments |
The preferred vertical slip rate is based on heights of two multi-event scarps on surfaces of known ages, and from the height of a single-event scarp that ended a recurrence interval of known duration (Machette and others, 1998). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Machette, M.N., Personius, S.F., Kelson, K.I., Haller, K.M., and Dart, R.L., 1998, Map and data for Quaternary faults and folds in New Mexico: U.S. Geological Survey Open-File Report 98-521, 443 p., 1 pl., scale 1:750,000. 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.
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