On Oct. 20. 1990, there occurred a earthquake with magnitude of 6.2 in Jingtai area, Gansu. which is main-aftershock type. The seismic active feature shows:before strong earthquake, the distribution pattern of moderate and small events changed, the seismic belt appeared impending main shock:the time fractal dimension value decreased and got the minimum, the position style of equo-distance distribution of earthquakes with magnitude of 6 occurred nearby was characterized by filling location obviously. Also. this paper suggested a new method to rapidly obtain the trend of seismic rupture and nodal face from the position of stations, relative to epicentre, with the maximum values of magnitude determined.
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阎志德,王周元.1990年10月20景泰地震的活动图象及其特征[J].地震工程学报,1992,14(2):42-48,58. Yan Zhide, Wang Zhouyuan. SEISMIC PATTERN AND CHARACTERISTICS OF THE JINGTAI EARTHQUAKE OF OCT. 20, 1990[J]. China Earthquake Engineering Journal,1992,14(2):42-48,58.