DYNAMIC ANALYSIS ON INTERACTION BETWEEN THEHAIYUAN-GULANG-CHANGMA GREAT EARTHQUAKE IN THE NORTH BOUNDARY OF THE TIBETAN PLATEAU
This paper has studied the interaction between theHaiyuan-Gulang-Changma gre at earthquake on the north boundary of the Tibetan plateau based on the concep tion of Coulomb static stress change. The results show that the Gulang earthqua ke occurred in advance of 16～44 years from triggering by Haiyuan event, and the occurrence of Changma earthquake was not affected by Coulomb static stress change resulting from Haiyuan and Gulang earthquake occurrence.
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