Publications
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Modifications to existing ground-motion prediction equations in light of new data Modifications to existing ground-motion prediction equations in light of new data
We compare our recent ground-motion prediction equations (GMPEs) for western North America (WNA; Boore and Atkinson, 2008 [BA08]) and eastern North America (ENA; Atkinson and Boore, 2006 [AB06]; Atkinson, 2008 [A08]) to newly available ground-motion data. Based on these comparisons, we suggest revisions to our GMPEs for both WNA and ENA. The revisions for WNA affect only those events...
Authors
G. Atkinson, D.M. Boore
Inversion of ground-motion data from a seismometer array for rotation using a modification of Jaeger's method Inversion of ground-motion data from a seismometer array for rotation using a modification of Jaeger's method
We develop a new way to invert 2D translational waveforms using Jaeger's (1969) formula to derive rotational ground motions about one axis and estimate the errors in them using techniques from statistical multivariate analysis. This procedure can be used to derive rotational ground motions and strains using arrayed translational data, thus providing an efficient way to calibrate the...
Authors
Wu-Cheng Chi, W.H.K. Lee, J.A.D. Aston, C.J. Lin, C.-C. Liu
Real-time seismic monitoring of structures: Data handling and case studies Real-time seismic monitoring of structures: Data handling and case studies
Within the last decade, advances in the acquisition, processing and transmission of data from real-time seismic monitoring systems has contributed to the growth in the number structures instrumented with such systems. An equally important factor for such growth can be attributed to the demands by stakeholders to find rapid answers to important questions related to the functionality (or...
Authors
Mehmet Celebi
Geology and petroleum potential of the Eurasia Basin Geology and petroleum potential of the Eurasia Basin
The Eurasia Basin petroleum province comprises the younger, eastern half of the Arctic Ocean, including the Cenozoic Eurasia Basin and the outboard part of the continental margin of northern Europe. For the USGS petroleum assessment (CARA), it was divided into four assessment units (AUs): the Lena Prodelta AU, consisting of the deep-marine part of the Lena Delta; the Nansen Basin Margin...
Authors
Thomas E. Moore, Janet K. Pitman
Overview of the 2010 Haiti earthquake Overview of the 2010 Haiti earthquake
The 12 January 2010 Mw 7.0 earthquake in the Republic of Haiti caused an estimated 300,000 deaths, displaced more than a million people, and damaged nearly half of all structures in the epicentral area. We provide an overview of the historical, seismological, geotechnical, structural, lifeline-related, and socioeconomic factors that contributed to the catastrophe. We also describe some...
Authors
Reginald DesRoches, Mary Comerio, Marc Eberhard, Walter Mooney, Glenn Rix
88 hours: The U.S. Geological Survey National Earthquake Information Center response to the March 11, 2011 Mw 9.0 Tohoku earthquake 88 hours: The U.S. Geological Survey National Earthquake Information Center response to the March 11, 2011 Mw 9.0 Tohoku earthquake
The M 9.0 11 March 2011 Tohoku, Japan, earthquake and associated tsunami near the east coast of the island of Honshu caused tens of thousands of deaths and potentially over one trillion dollars in damage, resulting in one of the worst natural disasters ever recorded. The U.S. Geological Survey National Earthquake Information Center (USGS NEIC), through its responsibility to respond to...
Authors
Gavin Hayes, Paul Earle, Harley Benz, David Wald, Richard Briggs
A Geo-referenced 3D model of the Juan de Fuca Slab and associated seismicity A Geo-referenced 3D model of the Juan de Fuca Slab and associated seismicity
We present a Geographic Information System (GIS) of a new 3-dimensional (3D) model of the subducted Juan de Fuca Plate beneath western North America and associated seismicity of the Cascadia subduction system. The geo-referenced 3D model was constructed from weighted control points that integrate depth information from hypocenter locations and regional seismic velocity studies. We used...
Authors
J.L. Blair, P.A. McCrory, D. Oppenheimer, F. Waldhauser
Key science issues in the central and eastern United States for the next version of the USGS National Seismic Hazard Maps Key science issues in the central and eastern United States for the next version of the USGS National Seismic Hazard Maps
The USGS National Seismic Hazard Maps are updated about every six years by incorporating newly vetted science on earthquakes and ground motions. The 2008 hazard maps for the central and eastern United States region (CEUS) were updated by using revised New Madrid and Charleston source models, an updated seismicity catalog and an estimate of magnitude uncertainties, a distribution of...
Authors
M.D. Peterson, C.S. Mueller
Regional correlations of VS30 averaged over depths less than and greater than 30 meters Regional correlations of VS30 averaged over depths less than and greater than 30 meters
Using velocity profiles from sites in Japan, California, Turkey, and Europe, we find that the time-averaged shear-wave velocity to 30 m (VS30), used as a proxy for site amplification in recent ground-motion prediction equations (GMPEs) and building codes, is strongly correlated with average velocities to depths less than 30 m (VSz, with z being the averaging depth). The correlations for...
Authors
David Boore, Eric M. Thompson, Heloise Cadet
Using the 2011 Mw9.0 Tohoku earthquake to test the Coulomb stress triggering hypothesis and to calculate faults brought closer to failure Using the 2011 Mw9.0 Tohoku earthquake to test the Coulomb stress triggering hypothesis and to calculate faults brought closer to failure
The 11 March 2011 Tohoku Earthquake provides an unprecedented test of the extent to which Coulomb stress transfer governs the triggering of aftershocks. During 11-31 March, there were 177 aftershocks with focal mechanisms, and so the Coulomb stress change imparted by the rupture can be resolved on the aftershock nodal planes to learn whether they were brought closer to failure. Numerous...
Authors
Shinji Toda, Jian Lin, Ross Stein
Liquefaction probability curves for surficial geologic deposits Liquefaction probability curves for surficial geologic deposits
Liquefaction probability curves that predict the probability of surface manifestations of earthquake-induced liquefaction are developed for 14 different types of surficial geologic units. The units consist of alluvial fan, beach ridge, river delta topset and foreset beds, eolian dune, point bar, flood basin, natural river and alluvial fan levees, abandoned river channel, deep-water lake...
Authors
Thomas Holzer, Thomas Noce, Michael Bennett
Geodetic slip model of the 2011 M9.0 Tohoku earthquake Geodetic slip model of the 2011 M9.0 Tohoku earthquake
The three-dimensional crustal displacement field as sampled by GPS is used to determine the coseismic slip of the 2011 M9.0 Tohoku Earthquake. We employ a spherically layered Earth structure and use a combination of onland GPS, out to ∼4000 km from the rupture, and offshore GPS, which samples the high-slip region on the interplate boundary along the Japan trench. Inversion of the...
Authors
Frederick Pollitz, Roland Burgmann, Paramesh Banerjee