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自1966年3月邢台大地震以来,特别是1976年7月28日发生唐山大地震以后,提到地震,人们便心有余悸,因此对深大断裂,尤其是大断裂交汇的地方可能发生大地震,疑虑很多。为此,我们将构造地貌学的理论应用于江苏的地震预测预报工作,取得了较好的结果。绝大多数人曾认为华东大地震将发生在郯庐大断裂带。华东地区断层很多,断层相交的地方也很多,那么到底哪些地方可能发生强地震。我们认为关键是要搞清断层近期有无活动、活动的能量、活动的性质及幅度等,而解决这些问题,构造地貌学最能发挥作用。如通过分析
Since the great earthquake in Xingtai in March 1966, especially after the Tangshan earthquake on July 28, 1976, people mentioned that there was a lingering fear of earthquakes. Therefore, a major earthquake may occur in deep faults, especially where large faults intersect. There are many doubts. To this end, we applied the theory of tectonic geomorphology to earthquake prediction in Jiangsu and achieved good results. The vast majority of people think that the Great East China Earthquake will occur in the Great Taichi fault zone. There are many faults in East China, and there are also many places where faults intersect. So where can a strong earthquake occur? We believe that the key is to find out whether or not there are recent activities in the fault, the energy of the activity, the nature and magnitude of the activity, etc. To solve these problems, structural geomorphology can play its best role. Such as through analysis