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Fault Name | State |
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Picuris-Pecos fault | New Mexico |
GEOMETRY | |
Dip (degrees) | 40/60/50 |
Dip direction | W |
Sense of slip | normal |
Rupture top (km) | 0 |
Rupture bottom (km) | 15 |
Rake (degrees) | -90 |
Length (km) | 99 |
MODEL VALUES | |
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Probability of activity | 1 |
Minimum magnitude | 6.5 |
Maximum magnitude | 7.39 |
b-value | 0.8 |
Assigned Dip | Fault-Parallel Slip Rate | Width | Annual Rate | a-value | Branch Weight |
---|---|---|---|---|---|
40 | 0.08 | 23.3 | 3.95e-05 | 0.881 | 0.2 |
50 | 0.07 | 19.6 | 2.78e-05 | 0.729 | 0.6 |
60 | 0.06 | 17.3 | 2.18e-05 | 0.622 | 0.2 |
Comments |
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The Picuris-Pecos fault was assigned a vertical slip rate of 0.05 mm/yr in the 1996 and subsequent national seismic-hazard maps. There were and still are no fault-specific data from which to calculate slip rates. Wong and others (1995) considered that a 5-m-high scarp would persist for only 100,000-150,000 years in the rugged terrane and moist climate of the surrounding Sangre de Christo Mountains. Accordingly, they considered a vertical slip rate of 0.05 mm/yr to be the upper bound of a long-term, average rate. Dip of fault changed to 50? based on redefined regional default value (Lund, 2006). |
Selected References |
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Wong, I., Kelson, K., Olig, S., Kolbe, T., Hemphill-Haley, M., Bott, J., Green, R., Kanakari, H., Sawyer, J., Silva, W., Stark, C., Haraden, C., Fenton, C., Unruh, J., Gardner, J., Reneau, S., and House, L., 1995, Seismic hazards evaluation of the Los Alamos National Laboratory: Technical report to Los Alamos National Laboratory, Los Alamos, New Mexico, February 24, 1995, 3 volumes, 12 pls., 16 appen. 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. |