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在归纳分析上海地区数十条浅层地震反射剖面中地震波组特点的基础上,通过与验证钻孔的比较,显示第四纪地层的各统底界可在相应的反射波组中得到反映
Based on the analysis of the characteristics of seismic waves in dozens of shallow seismic reflection profiles in Shanghai area and by comparison with the verified boreholes, it is shown that the universal boundaries of Quaternary strata can be reflected in the corresponding reflected wave groups