Publications
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Slip rate and slip magnitudes of past earthquakes along the Bogd left-lateral strike-slip fault (Mongolia)
We carried out morphotectonic studies along the left-lateral strike-slip Bogd Fault, the principal structure involved in the Gobi-Altay earthquake of 1957 December 4 (published magnitudes range from 7.8 to 8.3). The Bogd Fault is 260 km long and can be subdivided into five main geometric segments, based on variation in strike direction. West to East these segments are, respectively: the West Ih Bo
Authors
M. Rizza, J.-F. Ritz, R. Braucher, R. Vassallo, C. Prentice, Shannon A. Mahan, S. McGill, A. Chauvet, S. Marco, M. Todbileg, S. Demberel, D. Bourles
Liquefaction and other ground failures in Imperial County, California, from the April 4, 2010, El Mayor-Cucapah earthquake
The Colorado River Delta region of southern Imperial Valley, California, and Mexicali Valley, Baja California, is a tectonically dynamic area characterized by numerous active faults and frequent large seismic events. Significant earthquakes that have been accompanied by surface fault rupture and/or soil liquefaction occurred in this region in 1892 (M7.1), 1915 (M6.3; M7.1), 1930 (M5.7), 1940 (M6.9
Authors
Timothy P. McCrink, Cynthia L. Pridmore, John C. Tinsley, Robert R. Sickler, Scott J. Brandenberg, Jonathan P. Stewart
Developing seismogenic source models based on geologic fault data
Calculating seismic hazard usually requires input that includes seismicity associated with known faults, historical earthquake catalogs, geodesy, and models of ground shaking. This paper will address the input generally derived from geologic studies that augment the short historical catalog to predict ground shaking at time scales of tens, hundreds, or thousands of years (e.g., SSHAC 1997). A seis
Authors
Kathleen M. Haller, Roberto Basili
Comparison of main-shock and aftershock fragility curves developed for New Zealand and US buildings
Seismic risk assessment involves the development of fragility functions to express the relationship between ground motion intensity and damage potential. In evaluating the risk associated with the building inventory in a region, it is essential to capture 'actual' characteristics of the buildings and group them so that 'generic building types' can be generated for further analysis of their damage
Authors
S.R. Uma, H. Ryu, N. Luco, A.B. Liel, M. Raghunandan
Coastal subsidence in Oregon, USA during the giant Cascadia earthquake of AD 1700
Quantitative estimates of land-level change during the giant AD 1700 Cascadia earthquake along the Oregon coast are inferred from relative sea-level changes reconstructed from fossil foraminiferal assemblages preserved within the stratigraphic record. A transfer function, based upon a regional training set of modern sediment samples from Oregon estuaries, is calibrated to fossil assemblages in seq
Authors
A. D. Hawkes, B. P. Horton, A. R. Nelson, C. H. Vane, Y. Sawai
Improved earthquake monitoring in the central and eastern United States in support of seismic assessments for critical facilities
Evaluation of seismic monitoring capabilities in the central and eastern United States for critical facilities - including nuclear powerplants - focused on specific improvements to understand better the seismic hazards in the region. The report is not an assessment of seismic safety at nuclear plants. To accomplish the evaluation and to provide suggestions for improvements using funding from the A
Authors
William S. Leith, Harley M. Benz, Robert B. Herrmann
Albuquerque Seismological Laboratory--50 years of global seismology
The U.S. Geological Survey Albuquerque Seismological Laboratory is about 15 miles southeast of Albuquerque on the Pueblo of Isleta, adjacent to Kirtland Air Force Base. The Albuquerque Seismological Laboratory supports the Global Seismographic Network Program and the Advanced National Seismic System through the installation, operation, and maintenance of seismic stations around the world and serve
Authors
C. R. Hutt, Jon Peterson, Lind Gee, John Derr, Adam Ringler, David Wilson
Earthquakes in Mississippi and vicinity 1811-2010
This map summarizes two centuries of earthquake activity in Mississippi. Work on the Mississippi map was done in collaboration with the Mississippi Department of Environmental Quality, Office of Geology. The earthquake data plotted on the map are from several sources: the Mississippi Department of Environmental Quality, the Center for Earthquake Research and Information, the National Center for Ea
Authors
Richard L. Dart, Michael B. E. Bograd
Earthquakes in Arkansas and vicinity 1699-2010
This map summarizes approximately 300 years of earthquake activity in Arkansas. It is one in a series of similar State earthquake history maps. Work on the Arkansas map was done in collaboration with the Arkansas Geological Survey. The earthquake data plotted on the map are from several sources: the Arkansas Geological Survey, the Center for Earthquake Research and Information, the National Center
Authors
Richard L. Dart, Scott M. Ausbrooks
Three‐dimensional model for the crust and upper mantle in the Barents Sea region
The Barents Sea and its surroundings is an epicontinental region which previously has been difficult to access, partly because of its remote Arctic location (Figure 1) and partly because the region has been politically sensitive. Now, however, this region, and in particular its western parts, has been very well surveyed with a variety of geophysical studies, motivated in part by exploration for hy
Authors
H. Bangum, O. Ritzmann, N. Maercklin, J.I. Faleide, Walter D. Mooney, Shane T. Detweiler
Coseismic slip distribution of the February 27, 2010 Mw 8.9 Maule, Chile earthquake
[1] Static offsets produced by the February 27, 2010 Mw = 8.8 Maule, Chile earthquake as measured by GPS and InSAR constrain coseismic slip along a section of the Andean megathrust of dimensions 650 km (in length) × 180 km (in width). GPS data have been collected from both campaign and continuous sites sampling both the near-field and far field. ALOS/PALSAR data from several ascending and descendi
Authors
Fred F. Pollitz, Ben Brooks, Xiaopeng Tong, Michael G. Bevis, James H. Foster, Roland Burgmann