Comments |
Assigned vertical slip rate is based on 100 m offset of an early Quaternary basalt, dated at 1.4?0.3 Ma (Wenrich and others, 1995). From these data, P.A. Pearthree (written commun., 2002) calculated a slip rate of 0.06-0.09 mm/yr. We assigned the average of this range. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Wenrich, K.J., Billingsley, G.H., and Blackerby, B.A., 1995, Spatial migration and compositional changes of Miocene-Quaternary magmatism in the western Grand Canyon: Journal of Geophysical Research, v. 100, no. B7, p. 10,417-10,440. 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.
|