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Discussion of Some Problems in the Research into the Seismotectonics of Strong Earthquakes on the North China Plain

机译:华北平原强震地震构造研究中若干问题的讨论

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The tectonic characteristics and research problems of five earthquakes with M ≥ 7.0 on the North China Plain over the last 300 years are addressed in the paper, including the cognition that there were no ground fractures in the 1966 Xingtai earthquake, the question caused by the thrust activity of the seismic fault of the Tangshan Earthquake and the discussion of the seismotectonic environment of the 1830 Cixian earthquake and the 1937 Heze earthquake. The author thinks that the main reason for the problems in research of strong earthquake tectonics in the region is that the status of activity of the main tectonics during the Late Quaternary are unknown. This affects the founding of discrimination criteria for seismotectonics of strong earthquakes on the North China Plain. Discriminating the Holocene active faults from the large number of faults is the most effective method for seismic hazard assessment in the area in future.
机译:研究了华北平原近300年的5次M≥7.0级地震的构造特征和研究问题,包括认识到1966年的邢台地震中没有地裂缝,这是由推力引起的。唐山地震断层的活动和对1830年磁县地震和1937年菏泽地震的地震构造环境的讨论。作者认为,该地区强地震构造研究存在问题的主要原因是第四纪晚期主要构造活动的状态尚不清楚。这影响了华北平原强震地震构造判别标准的建立。区分全新世活动断层和大量断层是未来该地区地震危险性评估的最有效方法。

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