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

2006ES000208-fig12.html
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.

RJES

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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