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3D ground-motion simulations of M (sub w) 7 earthquakes on the Salt Lake City segment of the Wasatch fault zone; variability of long-period (T> or =1 s) ground motions and sensitivity to kinematic rupture parameters

Morgan P. Moschetti, Stephen Hartzell, Leonardo Ramirez-Guzman, Arthur D. Frankel, Stephen J. Angster and William J. Stephenson
3D ground-motion simulations of M (sub w) 7 earthquakes on the Salt Lake City segment of the Wasatch fault zone; variability of long-period (T> or =1 s) ground motions and sensitivity to kinematic rupture parameters
Bulletin of the Seismological Society of America (June 2017) 107 (4): 1704-1723

Abstract

We examine the variability of long-period (T> or =1 s) earthquake ground motions from 3D simulations of M (sub w) 7 earthquakes on the Salt Lake City segment of the Wasatch fault zone, Utah, from a set of 96 rupture models with varying slip distributions, rupture speeds, slip velocities, and hypocenter locations. Earthquake ruptures were prescribed on a 3D fault representation that satisfies geologic constraints and maintained distinct strands for the Warm Springs and for the East Bench and Cottonwood faults. Response spectral accelerations (SA; 1.5-10 s; 5% damping) were measured, and average distance scaling was well fit by a simple functional form that depends on the near-source intensity level SA (sub 0) (T) and a corner distance R (sub c) :SA(R,T)=SA (sub 0) (T)(1+(R/R (sub c) )) (super -1) . Period-dependent hanging-wall effects manifested and increased the ground motions by factors of about 2-3, though the effects appeared partially attributable to differences in shallow site response for sites on the hanging wall and footwall of the fault. Comparisons with modern ground-motion prediction equations (GMPEs) found that the simulated ground motions were generally consistent, except within deep sedimentary basins, where simulated ground motions were greatly underpredicted. Ground-motion variability exhibited strong lateral variations and, at some sites, exceeded the ground-motion variability indicated by GMPEs. The effects on the ground motions of changing the values of the five kinematic rupture parameters can largely be explained by three predominant factors: distance to high-slip subevents, dynamic stress drop, and changes in the contributions from directivity. These results emphasize the need for further characterization of the underlying distributions and covariances of the kinematic rupture parameters used in 3D ground-motion simulations employed in probabilistic seismic-hazard analyses. Electronic Supplement: Description of seismic-velocity model and wave propagation code and interpretation of directivity effects, and figures of fault geometry, Z1 and Z2.5 depths, effects of rupture speed variations on directivity effects and amplifications.


ISSN: 0037-1106
EISSN: 1943-3573
Coden: BSSAAP
Serial Title: Bulletin of the Seismological Society of America
Serial Volume: 107
Serial Issue: 4
Title: 3D ground-motion simulations of M (sub w) 7 earthquakes on the Salt Lake City segment of the Wasatch fault zone; variability of long-period (T> or =1 s) ground motions and sensitivity to kinematic rupture parameters
Affiliation: U. S. Geological Survey, Denver, CO, United States
Pages: 1704-1723
Published: 20170620
Text Language: English
Publisher: Seismological Society of America, Berkeley, CA, United States
References: 93
Accession Number: 2017-058789
Categories: Seismology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. sketch maps
N40°00'00" - N41°00'00", W111°30'00" - E112°30'00"
Secondary Affiliation: Universidad Nacional Autonoma de Mexico, MEX, Mexico
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2022, American Geosciences Institute. Abstract, Copyright, Seismological Society of America. Reference includes data from GeoScienceWorld, Alexandria, VA, United States
Update Code: 201731
Program Name: USGSOPNon-USGS publications with USGS authors
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