Comments |
Preferred vertical slip rate from dePolo (1998 #2845) and dePolo and Anderson (2000 #4471) based on an data presented by Bryant (1984 #2883). Bryant (1984 #2883) reports Holocene deposits offset up to 5.8 m; dePolo (1998 #2845) and dePolo and Anderson (2000 #4471) assumed an age of 4-12 ka (with a mean age of 8 ka) for the deposit. 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. Bryant, W.A., 1984, Evidence of recent faulting along the Antelope Valley fault zone, Mono County, California: California Division of Mines and Geology, Open-File Report 84-56, scale 1:48,000. dePolo, C.M., and Anderson, J.G., 2000, Estimating the slip rates of normal faults in the Great Basin, USA: Basin Research, v. 12, p. 227-240. 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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