Publications
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Seismic Station Installation Orientation Errors at ANSS and IRIS/USGS Stations Seismic Station Installation Orientation Errors at ANSS and IRIS/USGS Stations
Many seismological studies depend on the published orientations of sensitive axes of seismic instruments relative to north (e.g., Li et al., 2011). For example, studies of the anisotropic structure of the Earth’s mantle through SKS‐splitting measurements (Long et al., 2009), constraints on core–mantle electromagnetic coupling from torsional normal‐mode measurements (Dumberry and Mound...
Authors
Adam T. Ringler, Charles R. Hutt, K. Persfield, Lind S. Gee
Long-range hazard assessment of volcanic ash dispersal for a Plinian eruptive scenario at Popocatépetl volcano (Mexico): implications for civil aviation safety Long-range hazard assessment of volcanic ash dispersal for a Plinian eruptive scenario at Popocatépetl volcano (Mexico): implications for civil aviation safety
Popocatépetl is one of Mexico’s most active volcanoes threatening a densely populated area that includes Mexico City with more than 20 million inhabitants. The destructive potential of this volcano is demonstrated by its Late Pleistocene–Holocene eruptive activity, which has been characterized by recurrent Plinian eruptions of large magnitude, the last two of which destroyed human...
Authors
Rosanna Bonasia, Chirara Scaini, Lucia Capra, Manuel Nathenson, Claus Siebe, Lilia Arana-Salinas, Arnau Folch
Ca, Sr, O and D isotope approach to defining the chemical evolution of hydrothermal fluids: example from Long Valley, CA, USA Ca, Sr, O and D isotope approach to defining the chemical evolution of hydrothermal fluids: example from Long Valley, CA, USA
We present chemical and isotopic data for fluids, minerals and rocks from the Long Valley meteoric-hydrothermal system. The samples encompass the presumed hydrothermal upwelling zone in the west moat of the caldera, the Casa Diablo geothermal field, and a series of wells defining a nearly linear, ∼16 km long, west-to-east trend along the likely fluid flow path. Fluid samples were...
Authors
Shaun T. Brown, B. Mack Kennedy, Donald J. DePaolo, Shaul Hurwitz, William C. Evans
Seismotectonic framework of the 2010 February 27 Mw 8.8 Maule, Chile earthquake sequence Seismotectonic framework of the 2010 February 27 Mw 8.8 Maule, Chile earthquake sequence
After the 2010 Mw 8.8 Maule earthquake, an international collaboration involving teams and instruments from Chile, the US, the UK, France and Germany established the International Maule Aftershock Deployment temporary network over the source region of the event to facilitate detailed, open-access studies of the aftershock sequence. Using data from the first 9-months of this deployment...
Authors
Gavin P. Hayes, Eric Bergman, Kendra J. Johnson, Harley M. Benz, Lucy Brown, Anne S. Meltzer
Compaction and gas loss in welded pyroclastic deposits as revealed by porosity, permeability, and electrical conductivity measurements of the Shevlin Park Tuff Compaction and gas loss in welded pyroclastic deposits as revealed by porosity, permeability, and electrical conductivity measurements of the Shevlin Park Tuff
Pyroclastic flows produced by large volcanic eruptions commonly densify after emplacement. Processes of gas escape, compaction, and welding in pyroclastic-flow deposits are controlled by the physical and thermal properties of constituent material. Through measurements of matrix porosity, permeability, and electrical conductivity, we provide a framework for understanding the evolution of...
Authors
Heather M. Wright, Katharine V. Cashman
The Mw 5.8 Mineral, Virginia, earthquake of August 2011 and aftershock sequence: constraints on earthquake source parameters and fault geometry The Mw 5.8 Mineral, Virginia, earthquake of August 2011 and aftershock sequence: constraints on earthquake source parameters and fault geometry
The Mw 5.8 earthquake of 23 August 2011 (17:51:04 UTC) (moment, M0 5.7×1017 N·m) occurred near Mineral, Virginia, within the central Virginia seismic zone and was felt by more people than any other earthquake in United States history. The U.S. Geological Survey (USGS) received 148,638 felt reports from 31 states and 4 Canadian provinces. The USGS PAGER system estimates as many as 120...
Authors
Daniel E. McNamara, H.M. Benz, Robert B. Herrmann, Eric A. Bergman, Paul Earle, Anne Meltzer, Mitch Withers, Martin Chapman
HiRISE observations of new impact craters exposing Martian ground ice HiRISE observations of new impact craters exposing Martian ground ice
Twenty small new impact craters or clusters have been observed to excavate bright material inferred to be ice at mid and high latitudes on Mars. In the northern hemisphere, the craters are widely distributed geographically and occur at latitudes as low as 39°N. Stability modeling suggests that this ice distribution requires a long-term average atmospheric water vapor content around 25...
Authors
Colin M. Dundas, Shane Byrne, Alfred S. McEwen, Michael T. Mellon, Megan R. Kennedy, Ingrid J. Daubar, Lee Saper
A scenario study of seismically induced landsliding in Seattle using broadband synthetic seismograms A scenario study of seismically induced landsliding in Seattle using broadband synthetic seismograms
We demonstrate the value of utilizing broadband synthetic seismograms to assess regional seismically induced landslide hazard. Focusing on a case study of an Mw 7.0 Seattle fault earthquake in Seattle, Washington, we computed broadband synthetic seismograms that account for rupture directivity and 3D basin amplification. We then adjusted the computed motions on a fine grid for 1D...
Authors
Kate E. Allstadt, John E. Vidale, Arthur D. Frankel
Modeling earthquake rate changes in Oklahoma and Arkansas: possible signatures of induced seismicity Modeling earthquake rate changes in Oklahoma and Arkansas: possible signatures of induced seismicity
The rate of ML≥3 earthquakes in the central and eastern United States increased beginning in 2009, particularly in Oklahoma and central Arkansas, where fluid injection has occurred. We find evidence that suggests these rate increases are man‐made by examining the rate changes in a catalog of ML≥3 earthquakes in Oklahoma, which had a low background seismicity rate before 2009, as well as...
Authors
Andrea L. Llenos, Andrew J. Michael
The attenuation of Fourier amplitudes for rock sites in eastern North America The attenuation of Fourier amplitudes for rock sites in eastern North America
We develop an empirical model of the decay of Fourier amplitudes for earthquakes of M 3–6 recorded on rock sites in eastern North America and discuss its implications for source parameters. Attenuation at distances from 10 to 500 km may be adequately described using a bilinear model with a geometric spreading of 1/R1.3 to a transition distance of 50 km, with a geometric spreading of 1/R0...
Authors
Gail M. Atkinson, David M. Boore
Extreme ground motions and Yucca Mountain Extreme ground motions and Yucca Mountain
Yucca Mountain is the designated site of the underground repository for the United States' high-level radioactive waste (HLW), consisting of commercial and military spent nuclear fuel, HLW derived from reprocessing of uranium and plutonium, surplus plutonium, and other nuclear-weapons materials. Yucca Mountain straddles the western boundary of the Nevada Test Site, where the United...
Authors
Thomas C. Hanks, Norman A. Abrahamson, Jack W. Baker, David M. Boore, Mark Board, James N. Brune, C. Allin Cornell, John W. Whitney
Mechanical properties of simulated Mars materials: gypsum-rich sandstones and lapilli tuff Mechanical properties of simulated Mars materials: gypsum-rich sandstones and lapilli tuff
Observations by the Mars Exploration Rover (MER) Opportunity, and other recent studies on diagenesis in the extensive equatorial layered deposits on Mars, suggest that the likely lithologies of these deposits are gypsum-rich sandstones and tuffaceous sediments (for example, Murchie and others, 2009; Squyres and others, 2012; Zimbelman and Scheidt, 2012). Of particular interest is how the
Authors
Carolyn Morrow, David Lockner, Chris Okubo