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。
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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