Rapid Source Characterization of the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake

Earth, Planets and Space
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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. However, significant observations such as the up-dip nature of rupture propagation and the along-strike length of faulting did not significantly change, demonstrating the usefulness of rapid source characterization for understanding the first order characteristics of major earthquakes.

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Publication type Article
Publication Subtype Journal Article
Title Rapid Source Characterization of the 2011 Mw 9.0 off the Pacific coast of Tohoku Earthquake
Series title Earth, Planets and Space
DOI 10.5047/eps.2011.05.012
Volume 63
Issue 7
Year Published 2011
Language English
Publisher Springer
Contributing office(s) Geologic Hazards Science Center
Description 6 p.
First page 529
Last page 534
Time Range Start 2011-03-11
Time Range End 2011-03-11
Country Japan
Other Geospatial Tohoku, Honshu
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