Abstract
The Shanxi tectonic belt is a historically earthquakeabundant area. For the majority of strong earthquakes in this area, the distribution of earthquake foci was controlled by the N-S oriented local structures on the tectonic belt. Studies of the present stress state of the Shanxi tectonic belt can contribute to the understanding of the relationship between strong earth quakes' occurrence and their structural distribution and also facilitate assessments of regional seismic danger and determina tion of the regions wherein strong earthquakes may occur in future. Using the Cataclastic Analysis Method (CAM), we per formed stress inversion based on the focal mechanism data of earthquakes which took place in the Shanxi tectonic belt from 1967 to 2010. Our results show that orientations of the maximum principal compressive stress axis of the Shanxi tectonic belt might have been variable before and after the 2001 Kunlun MS=8.1 strong earthquake, with two different superior trends of the NW-SE and NE-SW orientation in different periods. When the maximum principal compressive stress axis is oriented in the NE-SW direction, the pattern of the space distribution of the seismic events in the Shanxi tectonic belt shows a trend of their concentration in the N-S oriented tectonic segments. At the same time, the stress state is registered as horizontal shea ring and horizontal extension in the N-S and NE-SW oriented local segments in turn. When the maximum principal com pressive stress axis is NW-SE oriented, the stress state of the N-S and NE-SW oriented tectonic segments is primarily regis tered as horizontal shearing. Estimations of plunges of stress axes show that seismicity in the Shanxi belt corresponds prima rily to the activity of lowangle faults, and highangle stress sites are located in the NE-SW oriented extensional tectonic seg ments of the Shanxi belt. This indicates that the stress change of the Shanxi belt is caused by adjustment of the regional stress field, rather than by the diverse seismic activities.
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