The key studied areas are the paishanlou , daban , dayintaogou , wujiazi gold deposits . in terms of the study of regional structures , geophysics , and geochemistry , and necessary tectono - physical and numerical modeling , as well as studies of ore - forming and ore - controlling structures , the author holds that the detached - ductile sheari ng zone of the metamorphic core complex is the main ore - controlling structural system , and the regional mineralization is related with the regional ore - forming structural systems which are controlled by compounding of regional structural systems with different time and grade 重点以排山楼、大板、大樱桃沟、五家子等金矿矿田构造调查为基础，以区域地质构造、地球物理、地球化学研究为背景，辅以成矿构造物理模型、数学模型，通过成矿构造、控矿构造研究，将本区金矿的成矿构造确认为变质核杂岩拆离滑脱剪切带，并且是与区域成矿构造系统相联系，在不同时期、不同级序、不同力学性质构造体系成分复合条件下成矿。
The author suggests that the three lithosphere - scale faults , lancangjiang fault , jinshanjiang - ailaoshan fault and axis fault in the middle of the basin , are the main geological structures that control the formation of basin , magmatism and metallogenic congregate district . the anticline structure with an axis of triassic strata and the related fault system within the basin , and gonglang arch - shaped folding structure in the south of the basin are the geological structure controlling the formation of ore fields . junctions of two or more faults with different orientation , interlayer cataclastic structural zone and oxidation - reduction ( redox ) boundary were the favorable position for the formation of ore bodies 认为澜沧江断裂、金沙江-哀牢山断裂及盆地中轴断裂这三条岩石圈断裂是主要的控盆-控岩(岩浆岩)构造及矿集区尺度的控矿构造；盆地中以三叠系为轴的背斜构造及相关的断裂系统、盆地西南缘公郎弧形构造等是矿田尺度的控矿构造；多组断裂的交叉、层间破碎带及地层柱中的氧化还原界面是形成矿体的有利部位。
