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研究了烧香河断裂附近的浅层人工地震资料，并结合其他有关资料，认为该断裂南部为中生代沉积盆地构造。同时，提出了烧香河断裂在新大地构造分区中的重要意义。
The shallow artificial seismic data near the Shaoxinghe fault are studied. Combined with other relevant data, it is considered that the southern part of the fault was a Mesozoic sedimentary basin. At the same time, the significance of the burning Xianghe fault in the structural division of the new earth is proposed.