Comments |
Preferred vertical slip rate is the average rate based on 21-37 m offsets of the 1.2 Ma Bandelier Tuff (Carter and Gardner, 1993; 1995). Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
Carter, K.E., and Gardner, J.N., 1995, Quaternary fault kinematics in the northwestern Española basin, Rio Grande rift, New Mexico, in Bauer, P.W., Kues, B.S., Dunbar, N.W., Karlstrom, K.E., and Harrison, B., eds., Geology of the Santa Fe region, New Mexico: New Mexico Geological Society, 46th Field Conference, September 27-30, 1995, Guidebook, p. 97-103. Carter, K.E., and Gardner, J.N., 1993, Quaternary fault kinematics in the northern Española basin, Rio Grande rift, New Mexico—Implications for early rift development: Eos, Transactions of the American Geophysical Union, v. 74, p. 611. 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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