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• W2100045117 abstract "Research Article| January 14, 2014 Frequency‐Dependent Seismic Attenuation in the Eastern United States as Observed from the 2011 Central Virginia Earthquake and Aftershock Sequence Daniel E. McNamara; Daniel E. McNamara aU.S. Geological Survey, MS966, Box 25046, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar Lind Gee; Lind Gee bU.S. Geological Survey, Albuquerque Seismological Laboratory, P.O. Box 82010, Albuquerque,New Mexico 87198‐2010 Search for other works by this author on: GSW Google Scholar Harley M. Benz; Harley M. Benz aU.S. Geological Survey, MS966, Box 25046, Denver, Colorado 80225 Search for other works by this author on: GSW Google Scholar Martin Chapman Martin Chapman cDepartment of Geosciences, 4044 Derring Hall, Virginia Tech, Blacksburg, Virginia 24061 Search for other works by this author on: GSW Google Scholar Bulletin of the Seismological Society of America (2014) 104 (1): 55–72. https://doi.org/10.1785/0120130045 Article history first online: 14 Jul 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Daniel E. McNamara, Lind Gee, Harley M. Benz, Martin Chapman; Frequency‐Dependent Seismic Attenuation in the Eastern United States as Observed from the 2011 Central Virginia Earthquake and Aftershock Sequence. Bulletin of the Seismological Society of America 2014;; 104 (1): 55–72. doi: https://doi.org/10.1785/0120130045 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of the Seismological Society of America Search Advanced Search Abstract Ground shaking due to earthquakes in the eastern United States (EUS) is felt at significantly greater distances than in the western United States (WUS) and for some earthquakes it has been shown to display a strong preferential direction. Shaking intensity variation can be due to propagation path effects, source directivity, and/or site amplification. In this paper, we use S and Lg waves recorded from the 2011 central Virginia earthquake and aftershock sequence, in the Central Virginia Seismic Zone, to quantify attenuation as frequency‐dependent Q(f). In support of observations based on shaking intensity, we observe high Q values in the EUS relative to previous studies in the WUS with especially efficient propagation along the structural trend of the Appalachian mountains. Our analysis of Q(f) quantifies the path effects of the northeast‐trending felt distribution previously inferred from the U.S. Geological Survey (USGS) “Did You Feel It” data, historic intensity data, and the asymmetrical distribution of rockfalls and landslides. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2100045117 date "2014-01-14" @default.
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• W2100045117 title "Frequency-Dependent Seismic Attenuation in the Eastern United States as Observed from the 2011 Central Virginia Earthquake and Aftershock Sequence" @default.
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• W2100045117 doi "https://doi.org/10.1785/0120130045" @default.
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