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Research Article| March 19, 2019 Comparison of Site Dominant Frequency from Earthquake and Microseismic Data in California Behzad Hassani; Behzad Hassani Corresponding Author aCivil Design, Generation Engineering, BC Hydro, 6911 Southpoint Drive, Edmonds A02, Burnaby, British Columbia, Canada V3N 4X8, Behzad.hassani@bchydro.com Search for other works by this author on: GSW Google Scholar Alan Yong; Alan Yong bDepartment of the Interior, U.S. Geological Survey, Earthquake Science Center, 525 South Wilson Avenue, Pasadena, California 91106 U.S.A., yong@usgs.gov Search for other works by this author on: GSW Google Scholar Gail M. Atkinson; Gail M. Atkinson cDepartment of Earth Sciences, Western University, 1151 Richmond Street, London, Ontario, Canada N6A 5B7, gmatkinson@aol.com Search for other works by this author on: GSW Google Scholar Tian Feng; Tian Feng dDepartment of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles E Young Drive East, Los Angeles, California 90024 U.S.A., tianfengseis@ucla.edu, meng@epss.ucla.edu Search for other works by this author on: GSW Google Scholar Lingsen Meng Lingsen Meng dDepartment of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles E Young Drive East, Los Angeles, California 90024 U.S.A., tianfengseis@ucla.edu, meng@epss.ucla.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Behzad Hassani Corresponding Author aCivil Design, Generation Engineering, BC Hydro, 6911 Southpoint Drive, Edmonds A02, Burnaby, British Columbia, Canada V3N 4X8, Behzad.hassani@bchydro.com Alan Yong bDepartment of the Interior, U.S. Geological Survey, Earthquake Science Center, 525 South Wilson Avenue, Pasadena, California 91106 U.S.A., yong@usgs.gov Gail M. Atkinson cDepartment of Earth Sciences, Western University, 1151 Richmond Street, London, Ontario, Canada N6A 5B7, gmatkinson@aol.com Tian Feng dDepartment of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles E Young Drive East, Los Angeles, California 90024 U.S.A., tianfengseis@ucla.edu, meng@epss.ucla.edu Lingsen Meng dDepartment of Earth, Planetary, and Space Sciences, University of California, Los Angeles, 595 Charles E Young Drive East, Los Angeles, California 90024 U.S.A., tianfengseis@ucla.edu, meng@epss.ucla.edu Publisher: Seismological Society of America First Online: 19 Mar 2019 Online Issn: 1943-3573 Print Issn: 0037-1106 © Seismological Society of America Bulletin of the Seismological Society of America (2019) 109 (3): 1034–1040. https://doi.org/10.1785/0120180267 Article history First Online: 19 Mar 2019 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Behzad Hassani, Alan Yong, Gail M. Atkinson, Tian Feng, Lingsen Meng; Comparison of Site Dominant Frequency from Earthquake and Microseismic Data in California. Bulletin of the Seismological Society of America 2019;; 109 (3): 1034–1040. doi: https://doi.org/10.1785/0120180267 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 An important predictive variable for site amplification is the site dominant frequency (fd). At seismic monitoring stations, fd can be calculated from the peak of the horizontal‐to‐vertical spectral ratios (HVSRs) obtained from earthquake recordings (eHVSR). For other sites, fd can be estimated from microseismic (mHVSR) observations. We compare the fd values derived from eHVSR (5% damped response spectra from the Next Generation Attenuation‐West2 NGA‐West2 database; Ancheta et al., 2014) with those derived from mHVSR (Fourier spectra from Yong et al., 2013) for seismic stations in California. We show that the logarithm of eHVSR fd scales linearly with the logarithm of mHVSR fd, with a standard deviation of 0.14log10 units for mHVSR fd larger than 0.2 Hz. The relationship holds for microseismic surveys at distances up to 300 m away from the seismic stations. The results of this study have beneficial implications for the characterization of site response in modern ground‐motion models as well as in building codes. You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
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