Publications
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Directivity of M 3.1 earthquake near Anza, California and the effect on peak ground motion Directivity of M 3.1 earthquake near Anza, California and the effect on peak ground motion
We show the effect of rupture directivity on peak ground‐motion values for a moderate magnitude event at Anza, California, and neighboring stations at the Imperial Valley. The event was located near Borrego Springs on the west side of the Salton Sea and was well recorded at broadband stations near Anza, California, and at stations on the west side of the Imperial Valley. After correcting...
Authors
Jon Peter B. Fletcher, John Boatwright
On the utilization of synthetic and measured earthquake ground motions for designing building monitoring systems in the near-field of major faults On the utilization of synthetic and measured earthquake ground motions for designing building monitoring systems in the near-field of major faults
Agencies and research groups engaged in studying measures for enhancing the resiliency of communities have recently placed emphasis on the need for extensive implementation of monitoring systems for rapid post-event assessment of structural integrity. Designing a monitoring system for a building requires a thorough knowledge of its potential nonlinear dynamic behavior with an associated
Authors
Floriana Petrone, David McCallen, Mehmet Celebi
Comment on “Interpretation of Kappa and fmax filters as source effect”, by Igor A. Beresnev Comment on “Interpretation of Kappa and fmax filters as source effect”, by Igor A. Beresnev
Beresnev (2019) advocates the use of an earthquake slip function that produces an ω-2.5 high-frequency falloff of Fourier displacement spectra in the far field, where ω denotes the angular frequency. He argues that the observed high-frequency decay of earthquake spectra can be adequately modeled by this ω-2.5 falloff, without needing to include high frequency attenuation at shallow depth...
Authors
Arthur D. Frankel
#EarthquakeAdvisory: Exploring discourse between government officials, news media and social media during the Bombay Beach 2016 Swarm #EarthquakeAdvisory: Exploring discourse between government officials, news media and social media during the Bombay Beach 2016 Swarm
Communicating probabilities of natural hazards to varied audiences is a notoriously difficult task. Many of these challenges were encountered during the 2016 Bombay Beach, California, swarm of ~100 2≤M≤4.3 earthquakes, which began on 26 September 2016 and lasted for several days. The swarm’s proximity to the southern end of the San Andreas fault caused concern that a larger earthquake...
Authors
Sara K. McBride, Andrea L. Llenos, Morgan T. Page, Nicholas van der Elst
Precision of VS30 values derived from noninvasive surface wave methods at 31 sites in California Precision of VS30 values derived from noninvasive surface wave methods at 31 sites in California
We study the inter- and intra-method variability of VS30 results by inverting/forward-modeling individual dispersion data for 31 seismographic stations located in California where combinations of surface-wave methods were applied and the minimum recorded wavelength from each method satisfies the 30-meter depth criteria. These methods consist of noninvasive geophysical (active and passive...
Authors
Alan K. Yong, Antony Martin, Jack Boatwright
The behavior of the Salesforce Tower, the tallest building in San Francisco, California inferred from earthquake and ambient shaking The behavior of the Salesforce Tower, the tallest building in San Francisco, California inferred from earthquake and ambient shaking
The newly constructed tallest building designed in conformance with performance-based design procedure in San Francisco, California is a 61-story building equipped with an accelerometric array that recorded the January 4, 2018 M4.4 Berkeley earthquake. The building is designed with concrete core shear walls and perimeter gravity steel columns. The earthquake records as well as on-demand...
Authors
Mehmet Celebi, Hamid Haddadi, Moh Huang, Michael Valley, John Hooper, Klemencic. Ron
The susceptibility of Oklahoma’s basement to seismic reactivation The susceptibility of Oklahoma’s basement to seismic reactivation
Recent widespread seismicity in Oklahoma is attributed to the reactivation of pre-existing, critically stressed and seismically unstable faults due to decades of wastewater injection. However, the structure and properties of the reactivated faults remain concealed by the sedimentary cover. Here, we explore the major ingredients needed to induce earthquakes in Oklahoma by characterizing...
Authors
Folarin Kolawole, C.S. Johnston, C.B. Morgan, Jefferson Chang, K Marfurt, David A. Lockner, Ze’ev Reches, B M Carpenter
The LArge-n Seismic Survey in Oklahoma (LASSO) experiment The LArge-n Seismic Survey in Oklahoma (LASSO) experiment
In 2016, the U.S. Geological Survey deployed more than 1,800 vertical-component nodal seismometers in Grant County, Oklahoma to study induced seismic activity associated with production of the Mississippi Limestone Play. The LArge-n Seismic Survey in Oklahoma (LASSO) array operated for approximately one month, covering a 25-km-by-32-km region with a nominal station spacing of ~400 m...
Authors
S. Dougherty, Elizabeth S. Cochran, R. M. Harrington
Late Quaternary slip rate of the Central Sierra Madre fault, southern California: Implications for slip partitioning and earthquake hazard Late Quaternary slip rate of the Central Sierra Madre fault, southern California: Implications for slip partitioning and earthquake hazard
The Sierra Madre fault system accommodates contraction within a large restraining bend area of the San Andreas fault along the northern margin of the Los Angeles metropolitan area in Southern California. Reverse slip along this fault system during earthquakes controls growth of the San Gabriel Mountains and poses a significant seismic hazard to the region. Here, we measure the late...
Authors
Reed J. Burgette, Austin Hanson, Katherine M. Scharer, Tammy M. Rittenour, Devin McPhillips
Coseismic slip and early afterslip of the M6.0 August 24, 2014 South Napa, California, earthquake Coseismic slip and early afterslip of the M6.0 August 24, 2014 South Napa, California, earthquake
We employ strong motion seismograms and static offsets from the Global Positioning System, Interferometric Synthetic Aperture Radar, and other measurements in order to derive a coseismic slip and afterslip model of the M6.0 24 August 2014 South Napa earthquake. This earthquake ruptured an ∼13‐km‐long portion of the West Napa fault with predominantly right‐lateral strike slip. In the...
Authors
Frederick Pollitz, Jessica R. Murray, Sarah E. Minson, Charles W. Wicks, Jerry L. Svarc, Benjamin A. Brooks
Responses of the odd couple Carquinez, CA, suspension bridge during the Mw6.0 south Napa earthquake of August 24, 2014 Responses of the odd couple Carquinez, CA, suspension bridge during the Mw6.0 south Napa earthquake of August 24, 2014
The behavior of the suspension bridge in Carquinez, CA, during the Mw6.0 24 August 2014 South Napa, CA earthquake is studied. Utilizing data from an extensive array of accelerometers that recorded the earthquake-excited motions, dynamic characteristics such as modes, corresponding frequencies and damping are identified and compared with previous studies that used ambient data of the deck...
Authors
Mehmet Celebi, S. Farid Ghahari, Ertugrul Taciroglu
Status of three-dimensional geological mapping and modeling activities in the U.S. Geological Survey Status of three-dimensional geological mapping and modeling activities in the U.S. Geological Survey
The U.S. Geological Survey (USGS), created in 1879, is the national geological survey for the United States and the sole science agency within its cabinet-level bureau, the Department of the Interior. The USGS has a broad mission, including: serving the Nation by providing reliable scientific information to describe and understand the Earth; minimize loss of life and property from...
Authors
Donald S. Sweetkind, Russell Graymer, D.K. Higley, Oliver S. Boyd