Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Craig M. dePolo"'
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
J. M. Bormann, Sean K Ahdi, A. M. Kell, Ian Pierce, Rachel L. Hatch, Ivan G. Wong, John N. Louie, Stephen J. Angster, Rachel E. Abercrombie, Graham M. Kent, John G. Anderson, Seth Dee, Kenneth D. Smith, William C. Hammond, James N. Brune, C. J. Ruhl, Stephen E. Dickenson, Corné Kreemer, Wanda J. Taylor, Michelle Elyse Dunn, James E. Faulds, Steven G. Wesnousky, Craig M. dePolo, Richard D. Koehler
Publikováno v:
Seismological Research Letters.
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Craig M. dePolo
Publikováno v:
Seismological Research Letters. 85:601-608
Sixty percent of magnitude 5.5 and larger earthquakes in the western Cordillera were preceded by foreshocks (Doser, 1989). Foreshocks also preceded the 2008 Wells ( M w 6.0; Smith et al. , 2011) and the 2008 Mogul ( M w 5.0; Smith et al. , 2008; dePo
Publikováno v:
Bulletin of the Seismological Society of America. 103:542-558
The extent to which faults exhibit temporally varying slip rates has important consequences for models of fault mechanics and probabilistic seismic hazard. Here, we explore the temporal behavior of the dextral‐slip Warm Springs Valley fault system,
Autor:
Craig M. dePolo, Christine M Ballard, Gary Johnson, Jordan T. Hastings, Linda D Goar, Heather Armeno, Ronald H. Hess, Jonathan G. Price
Publikováno v:
Environmental and Engineering Geoscience. 16:357-367
The Federal Emergency Management Agency9s loss-estimation model, HAZUS, is a powerful tool in emergency management. Its accuracy, when used immediately following an earthquake to estimate likely damage and effects, can be partially evaluated with sen
Publikováno v:
Environmental and Engineering Geoscience. 12:181-193
Several faults exposed in a 4- to 8-m-deep excavation in North Las Vegas exhibit evidence for two surface-faulting earthquakes that offset latest Pleistocene deposits and paleo-land surfaces about 2 to 3 m per event. These faults are secondary to a m
Publikováno v:
Bulletin of the Seismological Society of America. 93:2762-2768
The 1994 Double Spring Flat earthquake ( M W 5.8) occurred within a densely faulted step-over between the Genoa and Antelope Valley faults, two principal normal faults of the transition zone between the Basin and Range Province and the northern Sierr
Autor:
Dennis W. O'Leary, Robert B. Smith, John W. Whitney, Laurence W. Anderson, Robert R. Youngs, Susan S. Olig, Frank H. Swan, Christopher J. Fridrich, Silvio K. Pezzopane, R. Ernest Anderson, Ronald L. Bruhn, Albert M. Rogers, Kenneth D. Smith, David B. Slemmons, James C. Yount, Jon P. Ake, Gabriel R. Toro, Walter J. Arabasz, Kevin J. Coppersmith, James P. McCalpin, Peter L.K. Knuepfer, Craig M. dePolo, David P. Schwartz, Diane I. Doser, Alan R. Ramelli
Publikováno v:
Earthquake Spectra. 19:191-219
We present a methodology for conducting a site-specific probabilistic analysis of fault displacement hazard. Two approaches are outlined. The first relates the occurrence of fault displacement at or near the ground surface to the occurrence of earthq
Publikováno v:
Bulletin of the Seismological Society of America. 89:1458-1472
The Genoa fault, a principal normal fault of the transition zone between the Basin and Range Province and the northern Sierra Nevada, displays a large and conspicuous prehistoric scarp. Three trenches excavated across this scarp exposed two large-dis