Item talk:Q251520
From geokb
{
"USGS Publications Warehouse": { "@context": "https://schema.org", "@type": "Article", "additionalType": "Journal Article", "name": "Rapid Source Characterization of the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake", "identifier": [ { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse IndexID", "value": "70003856", "url": "https://pubs.usgs.gov/publication/70003856" }, { "@type": "PropertyValue", "propertyID": "USGS Publications Warehouse Internal ID", "value": 70003856 }, { "@type": "PropertyValue", "propertyID": "DOI", "value": "10.5047/eps.2011.05.012", "url": "https://doi.org/10.5047/eps.2011.05.012" } ], "journal": { "@type": "Periodical", "name": "Earth, Planets and Space", "volumeNumber": "63", "issueNumber": "7" }, "inLanguage": "en", "isPartOf": [ { "@type": "CreativeWorkSeries", "name": "Earth, Planets and Space" } ], "datePublished": "2011", "dateModified": "2021-01-07", "abstract": "On March 11th, 2011, a moment magnitude 9.0 earthquake struck off the coast of northeast Honshu, Japan, generating what may well turn out to be the most costly natural disaster ever. In the hours following the event, the U.S. Geological Survey National Earthquake Information Center led a rapid response to characterize the earthquake in terms of its location, size, faulting source, shaking and slip distributions, and population exposure, in order to place the disaster in a framework necessary for timely humanitarian response. As part of this effort, fast finite-fault inversions using globally distributed body- and surface-wave data were used to estimate the slip distribution of the earthquake rupture. Models generated within 7 hours of the earthquake origin time indicated that the event ruptured a fault up to 300 km long, roughly centered on the earthquake hypocenter, and involved peak slips of 20 m or more. Updates since this preliminary solution improve the details of this inversion solution and thus our understanding of the rupture process. 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