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1976年唐山大地震以后,在冀东平原引起了大规模的场地液化,其分布之广,形迹类型之多,规律性之强是前所未闻的。这次地震为我们提供了一个十分典型的地震工程地质研究现场。借助对各种震害规律以及不同类型地震液化震害效应的深入研究与分析,我们就有可能对震区进行正确的工程地质评价与分区,以便在强震地区重新规划建设之前,编制出各种专门性和预测性的地震工程地质图件,作为指导建筑工程及城市规划的布局与设计,以及采取必要的工程抗震
After the Great Tangshan Earthquake of 1976, a large-scale liquefaction of the site was caused in the Eastern Plain of the East China Sea. The distribution of the site was extensive, the types of trails were numerous, and the regularity was unheard of. This earthquake provided us with a very typical site for seismic engineering geological research. With the in-depth study and analysis of various earthquake damage laws and the effects of different types of seismic liquefaction and earthquake damage, we have the possibility to conduct correct engineering geology assessment and zoning for the earthquake regions so that we can formulate each before the re-planning and construction of strong earthquake regions. A specialized and predictable seismic engineering geological map as a guide to the layout and design of construction projects and urban planning, and to take necessary engineering anti-seismic