Comments |
Fossett (2005) calculates that the slip rate for this fault is 0.33 to 0.55 mm/yr based on trenching. Fossett and Taylor (2003) report a slip rate of 0.4 to 0.5 mm/yr based on the results of the same trenching study. The preferred vertical slip rate is less than the average of the publish slip rates because the above estimates are regarded as maxima in the original work. 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. Fossett, E., 2005, Paleoseismology of the Black Hills fault, southern Nevada, and implications for regional tectonics: University of Nevada, Las Vegas, unpublished Masters thesis, 94 p. Fossett, E. and Taylor, W.J., 2003, Evidence and implications of Holocene faulting along the Black Hills fault, southern Nevada: Geological Society of America, Abstracts with Program, v. 35, p. 476.
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