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通过地震资料特殊处理方法和湖上瞬变电磁方法（ＴＥＭ）的综合运用，确定了多项地震反射波动力学参数和地层电性参数，对断层内部及奥陶系灰岩充水的反映特征，对袁堂断层及其上升盘奥陶系灰岩的含水程度作出了定性评价。
Through the comprehensive application of special seismic data processing method and transient electromagnetic method (TEM) on the lake, a number of seismic reflection wave dynamic parameters and formation electrical parameters were identified, reflecting the water-filled characteristics of the interior of the fault and the Ordovician limestone. The quantitative evaluation of the water content of the Ordovician limestone in the Yuantang fault and its rising plateau.