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Science 20 May 2005:
Vol. 308. no. 5725, pp. 1133 - 1139
DOI: 10.1126/science.1112260

Research Articles

Rupture Process of the 2004 Sumatra-Andaman Earthquake

Charles J. Ammon,1* Chen Ji,2 Hong-Kie Thio,3 David Robinson,4 Sidao Ni,5,2 Vala Hjorleifsdottir,2 Hiroo Kanamori,2 Thorne Lay,6 Shamita Das,4 Don Helmberger,2 Gene Ichinose,3 Jascha Polet,7 David Wald8

The 26 December 2004 Sumatra-Andaman earthquake initiated slowly, with small slip and a slow rupture speed for the first 40 to 60 seconds. Then the rupture expanded at a speed of about 2.5 kilometers per second toward the north northwest, extending 1200 to 1300 kilometers along the Andaman trough. Peak displacements reached ~15 meters along a 600-kilometer segment of the plate boundary offshore of northwestern Sumatra and the southern Nicobar islands. Slip was less in the northern 400 to 500 kilometers of the aftershock zone, and at least some slip in that region may have occurred on a time scale beyond the seismic band.

1 Department of Geosciences, Pennsylvania State University, 440 Deike Building, University Park, PA 16802, USA.
2 Seismological Laboratory, California Institute of Technology, MS 252-21, Pasadena, CA 91125, USA.
3 URS Corporation, 566 El Dorado Street, Pasadena, CA 91101, USA.
4 Department of Earth Sciences, University of Oxford, Parks Road, Oxford OX1 3PR, UK.
5 Chinese Academy of Sciences Key Laboratory of Crust-Mantle Materials and Environments, University of Science and Technology of China, Hefei, Anhui 230026, China.
6 Earth Sciences Department and Institute of Geophysics and Planetary Physics, University of California, Santa Cruz, CA 95064, USA.
7 Institute for Crustal Studies, Santa Barbara, CA 93106, USA.
8 National Earthquake Information Center, U.S. Geological Survey (USGS), Golden, CO 80401, USA.

* To whom correspondence should be addressed. E-mail: cammon{at}geosc.psu.edu

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Science. ISSN 0036-8075 (print), 1095-9203 (online)