Tao Biaosheng. DISCUSSION ON THE CAUSATIVE STRUCTURE OF M=8.5 EARTHQUAKE IN HAIYUAN AND ITS STRESS FIELD[J]. North China Earthquake Sciences, 1986, 4(1): 48-55.
Citation:
Tao Biaosheng. DISCUSSION ON THE CAUSATIVE STRUCTURE OF M=8.5 EARTHQUAKE IN HAIYUAN AND ITS STRESS FIELD[J]. North China Earthquake Sciences, 1986, 4(1): 48-55.
Tao Biaosheng. DISCUSSION ON THE CAUSATIVE STRUCTURE OF M=8.5 EARTHQUAKE IN HAIYUAN AND ITS STRESS FIELD[J]. North China Earthquake Sciences, 1986, 4(1): 48-55.
Citation:
Tao Biaosheng. DISCUSSION ON THE CAUSATIVE STRUCTURE OF M=8.5 EARTHQUAKE IN HAIYUAN AND ITS STRESS FIELD[J]. North China Earthquake Sciences, 1986, 4(1): 48-55.
DISCUSSION ON THE CAUSATIVE STRUCTURE OF M=8.5 EARTHQUAKE IN HAIYUAN AND ITS STRESS FIELD
In this paper, the activity Since Quarternarly and characteristics of the causative fault zone, (mainly the causative fault zone of meizo-seismal region) the stress field and force source of Haiyuan earthquake in 1920 have been discussed. Based on this, two pieces of the important information about the occurence of Haiyuan earthquake are obtained.
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