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对康古尔塔格剪切带型金矿成矿体系地质地球化学特征研究后认为：①康古尔塔格金矿形成于脆韧性剪切变形和脆性变形阶段；②热液成矿反应体系包括成矿反应、控制反应及缓冲控制反应３类；③容矿构造活动方式有脆韧性缓冲转换作用、脆性破裂作用两种，前者构造环境有利于形成蚀变岩型矿化，后者则有利于形成石英脉状矿化；④成矿反应热力学性质和反应进行的程度——矿石品位受所处的地质环境和构造动力学条件的制约。
After studying the geo-geochemical characteristics of the Kanggutagen shear zone gold mineralization system, it is concluded that: ① the Kanggurtage gold deposit is formed during brittle-ductile shear deformation and brittle deformation; ② the hydrothermal mineralization reaction system Including ore-forming reactions, controlling reactions and buffer-controlled reactions. (3) There are two types of ore-hosting tectonism: brittle-ductile buffer conversion and brittle fracture. The former is conducive to the formation of altered rock mineralization and the latter has Conducive to the formation of quartz vein mineralization; ④ thermodynamic properties of the reaction and the extent of the reaction - ore grade is subject to the geological environment and tectonic dynamics constraints.