Item talk:Q262657
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{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Ground motions from induced earthquakes in Oklahoma and Kansas", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70201668", "url": "https://pubs.usgs.gov/publication/70201668" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70201668 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.1785/0220180200", "url": "https://doi.org/10.1785/0220180200" } ], "journal": { "@type": "Periodical", "name": "Seismological Research Letters", "volumeNumber": "90", "issueNumber": "1" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Seismological Research Letters" } ], "datePublished": "2018", "dateModified": "2019-01-28", "abstract": "Improved predictions of earthquake ground motions are critical to advancing seismic hazard analyses and earthquake response. The high seismicity rate from 2009 to 2016 in Oklahoma and Kansas provides an extensive data set for examining the ground motions from these events. We evaluate the ability of three suites of ground\u2010motion prediction equations (GMPEs)\u2014appropriate for modeling tectonic earthquakes in active crustal and stable continental regions\u2014to reproduce the observed ground motions. Mixed\u2010effects regressions are used to separate the ground\u2010motion residuals into bias, between\u2010event, and within\u2010event terms. Although the residuals depict differing accuracies in the ability of the three GMPE suites to predict the ground motions, some consistent trends emerge in the period, magnitude, and distance dependence. The trends suggest that aspects of the ground motions from these induced earthquakes are not well modeled by current tectonic GMPEs. Most important, we find evidence for relatively poor overall fit to the ground motions, by all of the GMPE suites, at periods less than about 0.2\u00a0s and above 3\u00a0s, greater\u2010than\u2010predicted magnitude scaling for small to moderate\u2010magnitude events (\u2060M\u22725\u2060), higher\u2010than\u2010predicted within\u2010event variability above 3\u00a0s, and an apparent geometric attenuation that is stronger than average predictions at close distances (\u2060R\u227220\u2009\u2009km) and short periods (\u2060T\u22721s). 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