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Kinematic Source Model of the 22 February 2011 Mw 6.2 Christchurch Earthquake Using Strong Motion Data
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EngineeringEarthquake HazardsEarthquake ScenarioEarth ScienceGeophysicsKinematic Source ModelEarthquake SourceMw 6.2Earthquake ForecastingGeodesyGround MotionEarthquake EngineeringInduced SeismicitySeismic ImagingGeographyEngineering GeologyFebruary 2011TectonicsSeismologyCivil EngineeringGeomechanicsEarth SciencesSeismic HazardDarfield Earthquake
Research Article| November 01, 2011 Kinematic Source Model of the 22 February 2011 Mw 6.2 Christchurch Earthquake Using Strong Motion Data Caroline Holden Caroline Holden GNS Science 1 Fairway Drive Lower Hutt Avalon 5010 New Zealand c.holden@gns.cri.nz Search for other works by this author on: GSW Google Scholar Seismological Research Letters (2011) 82 (6): 783–788. https://doi.org/10.1785/gssrl.82.6.783 Article history first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Caroline Holden; Kinematic Source Model of the 22 February 2011 Mw 6.2 Christchurch Earthquake Using Strong Motion Data. Seismological Research Letters 2011;; 82 (6): 783–788. doi: https://doi.org/10.1785/gssrl.82.6.783 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 The Canterbury earthquake sequence began in September 2010 with the Mw 7.1 (source: GeoNet catalog, http://geonet.org.nz/canterbury-quakes/) Darfield earthquake that ruptured the previously unknown 40-km-long Greendale fault 30 km west of Christchurch (Gledhill et al. 2011). Extreme ground accelerations as high as 1.8 g near the epicenter were recorded. The event caused intense liquefaction in the eastern suburbs of Christchurch as well as closer to downtown, near the course of the Avon River. The Darfield earthquake was followed by a major aftershock on 22 February local time (21 February UTC) of magnitude Mw 6.2 (source: GeoNet), but Me... 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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