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Bulletin of the Seismological Society of America; January 2007; v. 97; no. 1A; p. S174-S191; DOI: 10.1785/0120050630
© 2007 Seismological Society of America
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Crustal Deformation and Seismic History Associated with the 2004 Indian Ocean Earthquake: A Perspective from the Andaman–Nicobar Islands

C. P. Rajendran1, Kusala Rajendran1, R. Anu1, Anil Earnest*,1, Terry Machado1, P. M. Mohan2 and Jeffrey Freymueller3

1 Centre for Earth Science Studies
Akkulam, Trivandrum, India 695031
 (C.P.R., K.R., R.A., A.E., T.M.)
2 Centre for Ocean and Island Studies
Port Blair, India 744 101
 (P.M.M.)
3 Geophysical Institute
University of Alaska
Fairbanks, Alaska 99775
 (J.F.)

* Present address: CSIR Centre for Mathematical Modelling and Computer Simulation, Bangalore, India 560037.

The Indian Ocean earthquake of 26 December 2004 led to significant ground deformation in the Andaman and Nicobar region, accounting for ~800 km of the rupture. Part of this article deals with coseismic changes along these islands, observable from coastal morphology, biological indicators, and Global Positioning System (GPS) data. Our studies indicate that the islands south of 10° N latitude coseismically subsided by 1–1.5 m, both on their eastern and western margins, whereas those to the north showed a mixed response. The western margin of the Middle Andaman emerged by >1 m, and the eastern margin submerged by the same amount. In the North Andaman, both western and eastern margins emerged by >1 m. We also assess the pattern of long-term deformation (uplift/subsidence) and attempt to reconstruct earthquake/tsunami history, with the available data. Geological evidence for past submergence includes dead mangrove vegetation dating to 740 ± 100 yr B.P., near Port Blair and peat layers at 2–4 m and 10–15 m depths observed in core samples from nearby locations. Preliminary paleoseismological/tsunami evidence from the Andaman and Nicobar region and from the east coast of India, suggest at least one predecessor for the 2004 earthquake 900–1000 years ago. The history of earthquakes, although incomplete at this stage, seems to imply that the 2004-type earthquakes are infrequent and follow variable intervals.




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S. L. Bilek, K. Satake, and K. Sieh
Introduction to the Special Issue on the 2004 Sumatra-Andaman Earthquake and the Indian Ocean Tsunami
Bulletin of the Seismological Society of America, January 1, 2007; 97(1A): S1 - S5.
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