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肖板金矿床控矿构造是在变质岩构造基础上发育起来的蒲洋变质核杂岩构造之北西侧的剥离构造－低角度正断层系，具有产状平缓、延伸稳定、明显穿切变质岩片理等特征，为以压扭性为主的韧脆性变形，上盘向北西运动，构造岩以千枚岩或构造片岩为主。低角度断层是重要的储矿构造，其控制了矿体的形态、产状、规模和分布，其压扭性力学性质决定了交代为主的矿化蚀变类型，而且在成矿过程中也起到地球化学界面作用。
The ore-controlling structure of the Xiaopan gold deposit is a peel structure-low-angle normal fault system on the northwest side of the Puyang metamorphic core complex developed on the basis of the metamorphic rock structure. The ore-controlling structure of the Xiaopan gold deposit is smooth and stable in extension and obviously penetrated by cut- For the characteristics of ductile and brittle deformation, the upper plate moves to the northwest and the tectonic rocks are mainly phyllite or tectonic schist. The low-angle fault is an important ore deposit structure that controls the shape, occurrence, scale and distribution of the ore body. The mechanical properties of the compression-torsion determine the type of mineralization alteration that is mainly accountable. In the process of mineralization Play the role of geochemical interface.