断裂构造破碎带是该地区主要控矿、容矿构造。
The fault structural fracture zone is the main ore-control, ore-bearing structure.
通过这些明显的特征，可以很好地识别和判断构造破碎带。
By using these characteristics, the structure fractured zones can be identified and determined properly.
构造破碎带附近古生界底部和太古宇顶部出现破碎带，表现为高孔隙度、高渗透率带。
Near the décollement structure surface, at the bottom of the Cambrian and the top of the Archean, developed an interjacent fractured zone which shows high porosity and high permeability.
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