Publications
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Seismic hazard analysis using simulated ground motions Seismic hazard analysis using simulated ground motions
No abstract available.
Authors
M. Dabaghi, A. Der Kiureghian, S. Rezaeian, N. Luco
Ambient response of a unique performance-based design tall building with dynamic response modification features Ambient response of a unique performance-based design tall building with dynamic response modification features
A 64-story, performance-based design building with reinforced concrete core shear walls and unique dynamic response modification features (tuned liquid sloshing dampers and buckling-restrained braces) has been instrumented with a monitoring array of 72 channels of accelerometers. The responses of the building to ambient motions from ground or wind were recorded and analyzed to identify...
Authors
Mehmet Celebi, Moh Huang, Anthony Shakal, John Hooper, Ron Klemencic
Seismicity around Parkfield correlates with static shear stress changes following the 2003 Mw6.5 San Simeon earthquake Seismicity around Parkfield correlates with static shear stress changes following the 2003 Mw6.5 San Simeon earthquake
Earthquakes trigger other earthquakes, but the physical mechanism of the triggering is currently debated. Most studies of earthquake triggering rely on earthquakes listed in catalogs, which are known to be incomplete around the origin times of large earthquakes and therefore missing potentially triggered events. Here we apply a waveform matched-filter technique to systematically detect...
Authors
Xiaoteng Meng, Zhigang Peng, Jeanne L. Hardebeck
Holocene tectonics and fault reactivation in the foothills of the north Cascade Mountains, Washington Holocene tectonics and fault reactivation in the foothills of the north Cascade Mountains, Washington
We use LiDAR imagery to identify two fault scarps on latest Pleistocene glacial outwash deposits along the North Fork Nooksack River in Whatcom County, Washington (United States). Mapping and paleoseismic investigation of these previously unknown scarps provide constraints on the earthquake history and seismic hazard in the northern Puget Lowland. The Kendall scarp lies along the mapped...
Authors
Brian L. Sherrod, Elizabeth Barnett, Elizabeth Schermer, Harvey M. Kelsey, Jonathan Hughes, Franklin F. Foit, Craig S. Weaver, Ralph Haugerud, Tim Hyatt
ARRA-funded VS30 measurements using multi-technique approach at strong-motion stations in California and central-eastern United States ARRA-funded VS30 measurements using multi-technique approach at strong-motion stations in California and central-eastern United States
Funded by the 2009 American Recovery and Reinvestment Act (ARRA), we conducted geophysical site characterizations at 191 strong-motion stations: 187 in California and 4 in the Central-Eastern United States (CEUS). The geophysical methods used at each site included passive and active surface-wave and body-wave techniques. Multiple techniques were used at most sites, with the goal of...
Authors
Alan Yong, Antony Martin, Kenneth Stokoe, John Diehl
Finite-fault source inversion using teleseismic P waves: Simple parameterization and rapid analysis Finite-fault source inversion using teleseismic P waves: Simple parameterization and rapid analysis
We examine the ability of teleseismic P waves to provide a timely image of the rupture history for large earthquakes using a simple, 2D finite‐fault source parameterization. We analyze the broadband displacement waveforms recorded for the 2010 Mw∼7 Darfield (New Zealand) and El Mayor‐Cucapah (Baja California) earthquakes using a single planar fault with a fixed rake. Both of these...
Authors
C. Mendoza, S. Hartzell
Inferring fault rheology from low-frequency earthquakes on the San Andreas Inferring fault rheology from low-frequency earthquakes on the San Andreas
Families of recurring low-frequency earthquakes (LFEs) within nonvolcanic tremor (NVT) on the San Andreas fault in central California show strong sensitivity to shear stress induced by the daily tidal cycle. LFEs occur at all levels of the tidal shear stress and are in phase with the very small, ~400 Pa, stress amplitude. To quantitatively explain the correlation, we use a model from the...
Authors
Nicholas M. Beeler, Amanda Thomas, Roland Bürgmann, David R. Shelly
A domain decomposition approach to implementing fault slip in finite-element models of quasi-static and dynamic crustal deformation A domain decomposition approach to implementing fault slip in finite-element models of quasi-static and dynamic crustal deformation
We employ a domain decomposition approach with Lagrange multipliers to implement fault slip in a finite-element code, PyLith, for use in both quasi-static and dynamic crustal deformation applications. This integrated approach to solving both quasi-static and dynamic simulations leverages common finite-element data structures and implementations of various boundary conditions...
Authors
Brad T. Aagaard, M.G. Knepley, C.A. Williams
Insignificant solar-terrestrial triggering of earthquakes Insignificant solar-terrestrial triggering of earthquakes
We examine the claim that solar-terrestrial interaction, as measured by sunspots, solar wind velocity, and geomagnetic activity, might play a role in triggering earthquakes. We count the number of earthquakes having magnitudes that exceed chosen thresholds in calendar years, months, and days, and we order these counts by the corresponding rank of annual, monthly, and daily averages of...
Authors
Jeffrey J. Love, Jeremy N. Thomas
Field survey and damage assessment of the Mineral, Virginia, earthquake of August 23, 2011 Field survey and damage assessment of the Mineral, Virginia, earthquake of August 23, 2011
The town of Mineral, Virginia (Va.), underwent an M=5.8 earthquake on August 23, 2011. A U.S. Geological Survey team was sent to visually inspect and document the damage in the cities of Richmond, Charlottesville, Louisa, and Mineral, Va. Our inspection concluded that the Modified Mercalli Intensity rating of moderate (V) to very strong (VII) is consistent with the expected and observed...
Authors
Helen R. Thomas, Katharine Turkle
Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates Heterogeneous rupture in the great Cascadia earthquake of 1700 inferred from coastal subsidence estimates
Past earthquake rupture models used to explain paleoseismic estimates of coastal subsidence during the great A.D. 1700 Cascadia earthquake have assumed a uniform slip distribution along the megathrust. Here we infer heterogeneous slip for the Cascadia margin in A.D. 1700 that is analogous to slip distributions during instrumentally recorded great subduction earthquakes worldwide. The...
Authors
Pei-Ling Wang, Simon E. Engelhart, Kelin Wang, Andrea D. Hawkes, Benjamin P. Horton, Alan R. Nelson, Robert C. Witter
UNLV’s environmentally friendly Science and Engineering Building is monitored for earthquake shaking UNLV’s environmentally friendly Science and Engineering Building is monitored for earthquake shaking
The University of Nevada Las Vegas’ (UNLV) Science and Engineering Building is at the cutting edge of environmentally friendly design. As the result of a recent effort by the U.S. Geological Survey’s National Strong Motion Project in cooperation with UNLV, the building is now also in the forefront of buildings installed with structural monitoring systems to measure response during...
Authors
Erol Kalkan, Woody Savage, Shahneam Reza, Eric Knight, Ying Tian