RUSSIAN JOURNAL OF EARTH SCIENCES VOL. 8, ES5001, doi:10.2205/2006ES000208, 2006
[32] Animation 3 shows movements of blocks in the seismic source during the earthquakes. Calculations were made for the stressed state of blocks at the earthquakes preparatory stage. (see text for more detail).
[33] Animation 4 for the tsunami in the Indian Ocean of 26 December 2004 is based on the results of numerical simulation of surface waves generation for the seismic source consisting of 14 blocks (see [Hirata et al., 2006]). Movements of blocks in the seismic source were calculated for the stressed state of blocks, the propagation tsunami waves from seismic source was calculated up to 10-m isobath.
Citation: 2006), To analysis of source mechanism of the 26 December 2004 Indian Ocean tsunami, Russ. J. Earth Sci., 8, ES5001, doi:10.2205/2006ES000208.
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