This Paper introduces the earthquake and the geological situation in Arsnan region, on the base of which are discussed the formation of the structure and its development and the characteristics of the seismic deformation zone. It is considered that Shelifu Basin has been developed and shaped since Iate Cenozoic Era, NE Arsnan fault has been in a strong activities since Quarternary and this earthquake is the result of the continuous activities of this fault.
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陈志泰,才树华.阿斯南地震地质条件与地震形变带特征[J].地震工程学报,1987,9(1):74-82. Chen Zhitai, Cai Shuhua. GEOLOGICAL SITUATION AND CHARACTERISTCS OF SEISMIC DEFORMATION ZONE OF ARSNAN EARTHQUAKE[J]. China Earthquake Engineering Journal,1987,9(1):74-82.