Comments |
The preferred vertical slip rate is based on 300 m of vertical offset of the 0.63 Ma Lava Creek Tuff in the southern section of the fault. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Locke, W.W., Meyer, G.A., and Pings, J.C., 1992, Morphology of a postglacial fault scarp across the Yellowstone (Wyoming) caldera margin and its implications: Bulletin of the Seismological Society of America, v. 82, p. 511-516. 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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