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本文首先扼要的阐述了保存在山西省临汾县大阳公社东堡村匼河组地层中的形变现象,是地震造成的。然后,结合实际论证了喷砂管中的板瓦片是地震时掉入其中的,从而证明该形变现象是临汾1695年大地震的遗迹。在此基础上,根据该遗迹的规模和特征,文中还讨论了这次大震的震中、烈度和震级,并对该地震的发震构造进行了分析。最后,作者对震区快速上升的可能性提出了自己的见解。
This article first briefly describes the deformations in the stratum of Qunhe Formation of Dongpu Village, Dayang commune, Linfen County, Shanxi Province, which is caused by the earthquake. Then, the paper proves that the slab in the sand blast pipe falls into the earthquake during the earthquake, which proves that the deformation is the relic of the 1695 earthquake in Linfen. On this basis, according to the scale and characteristics of the relics, the epicenter, intensity and magnitude of the earthquake are also discussed, and the seismogenic structure of the earthquake is analyzed. Finally, the author put forward his opinion on the possibility of the rapid rise of the earthquake zone.