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Helping safeguard Veterans Affairs' hospital buildings by advanced earthquake monitoring Helping safeguard Veterans Affairs' hospital buildings by advanced earthquake monitoring

In collaboration with the U.S. Department of Veterans Affairs (VA), the National Strong Motion Project of the U.S. Geological Survey has recently installed sophisticated seismic systems that will monitor the structural integrity of hospital buildings during earthquake shaking. The new systems have been installed at more than 20 VA medical campuses across the country. These monitoring...
Authors
Erol Kalkan, Krishna Banga, Hasan S. Ulusoy, Jon Peter B. Fletcher, William S. Leith, James L. Blair

Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone Turbidite event history—Methods and implications for Holocene paleoseismicity of the Cascadia subduction zone

Turbidite systems along the continental margin of Cascadia Basin from Vancouver Island, Canada, to Cape Mendocino, California, United States, have been investigated with swath bathymetry; newly collected and archive piston, gravity, kasten, and box cores; and accelerator mass spectrometry radiocarbon dates. The purpose of this study is to test the applicability of the Holocene turbidite...
Authors
Chris Goldfinger, C. Hans Nelson, Ann E. Morey, Joel E. Johnson, Jason R. Patton, Eugene B. Karabanov, Julia Gutierrez-Pastor, Andrew T. Eriksson, Eulalia Gracia, Gita Dunhill, Randolph J. Enkin, Audrey Dallimore, Tracy Vallier

Initial assessment of the intensity distribution of the 2011 Mw5.8 Mineral, Virginia, earthquake Initial assessment of the intensity distribution of the 2011 Mw5.8 Mineral, Virginia, earthquake

The intensity data collected by the U.S. Geological Survey (USGS) "Did You Feel It?" (DYFI) Website (USGS, DYFI; http://earthquake.usgs.gov/earthquakes/dyfi/events/se/082311a/us/index.html, last accessed Sept 2011) for the Mw5.8 Mineral, Virginia, earthquake, are unprecedented in their spatial richness and geographical extent. More than 133,000 responses were received during the first...
Authors
Susan E. Hough

Source parameters of microearthquakes on an interplate asperity off Kamaishi, NE Japan over two earthquake cycles Source parameters of microearthquakes on an interplate asperity off Kamaishi, NE Japan over two earthquake cycles

We have estimated the source parameters of interplate earthquakes in an earthquake cluster off Kamaishi, NE Japan over two cycles of M~ 4.9 repeating earthquakes. The M~ 4.9 earthquake sequence is composed of nine events that occurred since 1957 which have a strong periodicity (5.5 ± 0.7 yr) and constant size (M4.9 ± 0.2), probably due to stable sliding around the source area (asperity)...
Authors
Naoki Uchida, Toru Matsuzawa, William L. Ellsworth, Kazutoshi Imanishi, Kouhei Shimamura, Akira Hasegawa

Probabilistic estimates of surface coseismic slip and afterslip for Hayward fault earthquakes Probabilistic estimates of surface coseismic slip and afterslip for Hayward fault earthquakes

We examine the partition of long‐term geologic slip on the Hayward fault into interseismic creep, coseismic slip, and afterslip. Using Monte Carlo simulations, we compute expected coseismic slip and afterslip at three alinement array sites for Hayward fault earthquakes with nominal moment magnitudes ranging from about 6.5 to 7.1. We consider how interseismic creep might affect the...
Authors
Brad T. Aagaard, James J. Lienkaemper, David P. Schwartz

Linear complementarity formulation for 3D frictional sliding problems Linear complementarity formulation for 3D frictional sliding problems

Frictional sliding on quasi-statically deforming faults and fractures can be modeled efficiently using a linear complementarity formulation. We review the formulation in two dimensions and expand the formulation to three-dimensional problems including problems of orthotropic friction. This formulation accurately reproduces analytical solutions to static Coulomb friction sliding problems...
Authors
J. Ole Kaven, Stephen H. Hickman, Nicholas C. Davatzes, Ovunc Mutlu

Correlation of clayey gouge in a surface exposure of the San Andreas fault with gouge at depth from SAFOD: Implications for the role of serpentinite in fault mechanics Correlation of clayey gouge in a surface exposure of the San Andreas fault with gouge at depth from SAFOD: Implications for the role of serpentinite in fault mechanics

Magnesium-rich clayey gouge similar to that comprising the two actively creeping strands of the San Andreas Fault in drill core from the San Andreas Fault Observatory at Depth (SAFOD) has been identified in a nearby outcrop of serpentinite within the fault zone at Nelson Creek. Each occurrence of the gouge consists of porphyroclasts of serpentinite and sedimentary rocks dispersed in a...
Authors
Diane E. Moore, Michael J. Rymer

Logs and data from trenches across and near the Green Valley Fault at the Mason Road site, Fairfield, Solano County, California, 2006-2009 Logs and data from trenches across and near the Green Valley Fault at the Mason Road site, Fairfield, Solano County, California, 2006-2009

The primary purpose of this report is to provide drafted field logs of exploratory trenches excavated across the Green Valley Fault in 2007 and 2009 that show evidence for four surface rupturing earthquakes in the past one thousand years. The site location and site detail are shown on sheet 1. The trench logs are shown on sheets 1, 2, and 3. We also provide radiocarbon laboratory dates...
Authors
James J. Lienkaemper, Robert R. Sickler, Shannon Mahan, Johnathan Brown, Liam M. Reidy, Mindy A. Kimball

LiDAR and field observations of slip distribution for the most recent surface ruptures along the central San Jacinto fault LiDAR and field observations of slip distribution for the most recent surface ruptures along the central San Jacinto fault

We measured offsets on tectonically displaced geomorphic features along 80 km of the Clark strand of the San Jacinto fault (SJF) to estimate slip‐per‐event for the past several surface ruptures. We identify 168 offset features from which we make over 490 measurements using B4 light detection and ranging (LiDAR) imagery and field observations. Our results suggest that LiDAR technology is...
Authors
J.B. Salisbury, T.K. Rockwell, T.J. Middleton, Kenneth W. Hudnut

Evaluation of fault-normal/fault-parallel directions rotated ground motions for response history analysis of an instrumented six-story building Evaluation of fault-normal/fault-parallel directions rotated ground motions for response history analysis of an instrumented six-story building

According to regulatory building codes in United States (for example, 2010 California Building Code), at least two horizontal ground-motion components are required for three-dimensional (3D) response history analysis (RHA) of buildings. For sites within 5 km of an active fault, these records should be rotated to fault-normal/fault-parallel (FN/FP) directions, and two RHA analyses should...
Authors
Erol Kalkan, Neal S. Kwong

Real-time seismic monitoring of instrumented hospital buildings Real-time seismic monitoring of instrumented hospital buildings

In collaboration with the Department of Veterans Affairs (VA), the U.S. Geological Survey's National Strong Motion Project has recently installed sophisticated seismic monitoring systems to monitor the structural health of two hospital buildings at the Memphis VA Medical Center in Tennessee. The monitoring systems in the Bed Tower and Spinal Cord Injury buildings combine sensing...
Authors
Erol Kalkan, Jon Peter B. Fletcher, William S. Leith, William S. McCarthy, Krishna Banga

Using pad‐stripped acausally filtered strong‐motion data Using pad‐stripped acausally filtered strong‐motion data

Most strong‐motion data processing involves acausal low‐cut filtering, which requires the addition of sometimes lengthy zero pads to the data. These padded sections are commonly removed by organizations supplying data, but this can lead to incompatibilities in measures of ground motion derived in the usual way from the padded and the pad‐stripped data. One way around this is to use the...
Authors
David Boore, Aida Azari Sisi, Sinan Akkar
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