RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES5001, doi:10.2205/2006ES000208, 2006

Figure 12. Modelling of the source of tsunamigenic earthquake 26 December 2004 by
motion of three keyboard blocks rising along the subduction zone one after
another from south to the north (a); space-time picture of the moving shoreline(b).
Maximum run-up is equal to
R max = 9.5 m, run-down
R min = 7.5 m.

Citation: Lobkovsky, L. I., R. Kh. Mazova, I. A. Garagash, L. Yu. Kataeva, and I. Nardin (2006), To analysis of source mechanism of the 26 December 2004 Indian Ocean tsunami, Russ. J. Earth Sci., 8, ES5001, doi:10.2205/2006ES000208.
Copyright 2006 by the Russian Journal of Earth Sciences
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