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Rapid Finite-source Analysis and Near-fault Strong Ground Motions: Application to the 2003 Mw 6.5 San Simeon and 2004 Mw 6.0 Parkfield Earthquakes
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2005
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EngineeringMw 6.5Earthquake HazardsEarth ScienceGeophysicsParkfield EarthquakesEarthquake SourceGeoenvironmental EngineeringGround MotionEarthquake EngineeringSeismic CycleInduced SeismicitySeismic ImagingEarthquake RuptureEngineering GeologySan SimeonTectonicsStructural GeologySeismologyCivil EngineeringGeomechanicsEarth SciencesRapid Finite-source AnalysisSeismic Hazard
Research Article| January 01, 2005 Rapid Finite-source Analysis and Near-fault Strong Ground Motions: Application to the 2003 Mw 6.5 San Simeon and 2004 Mw 6.0 Parkfield Earthquakes Douglas S. Dreger; Douglas S. Dreger Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Search for other works by this author on: GSW Google Scholar Lind Gee; Lind Gee Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Search for other works by this author on: GSW Google Scholar Peter Lombard; Peter Lombard Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Search for other works by this author on: GSW Google Scholar Mark H. Murray; Mark H. Murray Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Search for other works by this author on: GSW Google Scholar Barbara Romanowicz Barbara Romanowicz Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Search for other works by this author on: GSW Google Scholar Author and Article Information Douglas S. Dreger Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Lind Gee Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Peter Lombard Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Mark H. Murray Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Barbara Romanowicz Berkeley Seismological Laboratory University of California 281 McCone Hall Berkeley, CA 94720 dreger@seismo.berkeley.edu Publisher: Seismological Society of America First Online: 09 Mar 2017 Online ISSN: 1938-2057 Print ISSN: 0895-0695 © 2005 by the Seismological Society of America Seismological Research Letters (2005) 76 (1): 40–48. https://doi.org/10.1785/gssrl.76.1.40 Article history First Online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation Douglas S. Dreger, Lind Gee, Peter Lombard, Mark H. Murray, Barbara Romanowicz; Rapid Finite-source Analysis and Near-fault Strong Ground Motions: Application to the 2003 Mw 6.5 San Simeon and 2004 Mw 6.0 Parkfield Earthquakes. Seismological Research Letters 2005;; 76 (1): 40–48. doi: https://doi.org/10.1785/gssrl.76.1.40 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 SocietySeismological Research Letters Search Advanced Search Rapid characterization of near-fault strong ground shaking is essential for assessment of an earthquake's impact, including the scale of damage and loss. ShakeMap (Wald et al., 1999a) was developed as a tool for this purpose. To generate a ShakeMap, observed peak and spectral ground motion, as well as estimated instrumental intensity (Wald et al., 1999b), are interpolated with a model of ground-motion attenuation to produce contour maps of the various parameters. In California, the California Integrated Seismic Network (CISN) automatically produces ShakeMaps for moderate to large events within several minutes of their occurrence. ShakeMaps... 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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