Aftershock of the September 16, 1978 Tabas earthquake located from close-in observations madeduring a four-week fielding of temporary stations have been analyzed for the purpose of delineating detailed source geometry of the 1978 earthquake. Spatial distribution of aftershocks and their composite focal mechanism suggest that the geometry of faulting is far from planar. Aftershocks define two prominent alignment. The southern alignment strikes E-W to WNW-ESE, whereas the northern alignment strikes in a N-S to NNW-SSE direction with an abrupt change of nearly 50-60 degrees 33.4°N latitude. Both field observations and of surface faulting pattern and systematic variation of principal directions of stress axes computed from aftershock focal mechanism are consistent with the up-thrusting and imbrications of a wedge shaped crustal block with the wedge angle of about 120 degrees. Both geological and seismological evidence suggest that the deformed zone is truncated at the southern edge by preexisting E-W fault structures. New observations may provide a partial answer to the unexplained farfield asymmetry of the long period Rayleigh wave relation pattern recently observed for the mainshock across IDA network.

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