Earthquake in a Maze: Compressional Rupture Branching During the 2012 M w 8.6 Sumatra Earthquake

Author:

Meng L.1,Ampuero J.-P.1,Stock J.1,Duputel Z.1,Luo Y.1,Tsai V. C.1

Affiliation:

1. Seismological Laboratory, Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA.

Abstract

Earthquake in a Maze The 11 April 2012 magnitude 8.6 earthquake offshore of Sumatra was the largest measured earthquake along a strike-slip boundary that modern seismological instruments have ever recorded. Despite its size and proximity to a large population, there was no subsequent tsunami and there were no reported fatalities. Meng et al. (p. 724 , published online 19 July) used teleseismic data from seismological networks in Japan and Europe to image the source of high-frequency radiation generated by the earthquake to understand the mechanics of this unique event. The resultant back projections showed that the earthquake slowly ruptured along a complex series of faults. The deeper-than-usual rupture path and large stress drop are both features that may not be unique to this earthquake, suggesting that regions in a similar tectonic environment may have the potential for more complex—or larger—intraplate earthquakes than might have been expected.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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