Ｎ－Ｓ向断裂带与Ｅ－Ｗ向断裂带是崎峰茶－得田沟金矿田内主要赋矿构造带，具有韧－脆性变形特征；金的矿化富集与断裂带中糜棱岩及石英脉的发育密切相关；矿体定位于断裂带形变相变相对强烈的部位或区段。 N-S fracture zone and E-W fracture zone are the Qifengcha-Detiangou gold ore field and are characterized by ductile-brittle deformation. The mineralization of gold and the mylonite in the fault zone And the development of quartz veins are closely related to each other. The orebody is located in the site or section where the deformation of the deformation zone is relatively strong.