Comments |
The preferred vertical slip rate is based on data presented by Stickney and Bartholomew (1987) and Bartholomew and others (1999) that suggest there is 4-5 m of offset of inferred upper (<150 ka) Quaternary deposits. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Bartholomew, M.J., Stickney, M.C., and Wasklewicz, T.A., 2004, Interaction between the northern Basin and Range and the Yellowstone stress fields near the Red Rock fault, southwestern Montana: Geological Society of America Abstracts with Programs, v. 36, no. 4, p. 12. 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. Stickney, M.C., and Bartholomew, M.J., 1987, Seismicity and late Quaternary faulting of the northern Basin and Range province, Montana and Idaho: Bulletin of the Seismological Society of America, v. 77, p. 1602-1625.
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