In the east part of the orefield, the trend of arcual fault is convergent NNW-wards and divergent SE-wards. These arcual faults must be a broomlike structure.
矿区东部断裂呈弧形弯曲，并作NNW向收敛、SE方向撒开趋势，这些弧形断裂应是一帚状构造。
Divergent views exist as to the magnitude of displacement of the fault zone and more studies are needed.
关于郯庐断裂的平移距离仍存在着较大的分歧与有待深入研究之处。
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