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• W2890212577 abstract "Research Article| September 11, 2018 The 19 September 2017 M 7.1 Puebla‐Morelos Earthquake: Spectral Ratios Confirm Mexico City Zoning Mehmet Çelebi; Mehmet Çelebi aEarthquake Science Center, U.S. Geological Survey, Menlo Park, California 94025, celebi@usgs.gov Search for other works by this author on: GSW Google Scholar Valerie J. Sahakian; Valerie J. Sahakian bDepartment of Earth Sciences, University of Oregon, Eugene, Oregon 97403dAlso at Department of Earth Sciences, University of Oregon, Eugene, Oregon 97403. Search for other works by this author on: GSW Google Scholar Diego Melgar; Diego Melgar bDepartment of Earth Sciences, University of Oregon, Eugene, Oregon 97403 Search for other works by this author on: GSW Google Scholar Luis Quintanar Luis Quintanar cUniversidad Nacional Autónoma de México (UNAM), Instituto de Geofísica, 04510 CDMX, Mexico, luisq@igeofisica.unam.mx Search for other works by this author on: GSW Google Scholar Bulletin of the Seismological Society of America (2018) 108 (6): 3289–3299. https://doi.org/10.1785/0120180100 Article history first online: 11 Sep 2018 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Mehmet Çelebi, Valerie J. Sahakian, Diego Melgar, Luis Quintanar; The 19 September 2017 M 7.1 Puebla‐Morelos Earthquake: Spectral Ratios Confirm Mexico City Zoning. Bulletin of the Seismological Society of America 2018;; 108 (6): 3289–3299. doi: https://doi.org/10.1785/0120180100 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 One important element of understanding basin response to strong shaking is the analysis of spectral ratios, which may provide information about the dominant frequency of ground motion at specific locations. Spectral ratios computed from accelerations recorded by strong‐motion stations in Mexico City during the mainshock of the 19 September 2017 M 7.1 Puebla‐Morelos earthquake reveal predominate periods consistent with those mapped in the 2004 Mexican seismic design code. Furthermore, the predominant periods thus computed validate those studies using mainshock and aftershock recordings of the handful strong‐motion stations that recorded the 19 September 1985 M 8.1 Michoacán earthquake. Even though the number of stations in each of the zones (zones I, II, IIIa, b, c, and d) is not the same, they still allow confirmation of site frequencies (periods) attributable to the specific zones (particularly those in zones IIIa, b, c, and d). Spectral ratios are computed with two different methods: (1) horizontal to horizontal (H/H) ratio of smoothed amplitude spectrum of a horizontal channel in direction X of a station with respect to the smoothed amplitude spectrum of the horizontal channel in the same X direction of a reference stiff soil (or rock) station and (2) horizontal to vertical (H/V) ratio (or also known as the Nakamura method) of both horizontal (H) and vertical (V) channels of the same station. We show a comparison of the identified frequencies (periods) derived by both methods and find they are very similar and in good agreement with those indicated in the zoning maps of Mexico City in the 2004 seismic design code. 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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• W2890212577 date "2018-09-11" @default.
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• W2890212577 title "The 19 September 2017 M 7.1 Puebla‐Morelos Earthquake: Spectral Ratios Confirm Mexico City Zoning" @default.
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