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烧锅营子金矿区按含金矿脉排列、矿脉构造、产生条件、矿石组合和建造，可将矿脉划分为石英脉型、蚀变岩型、复合脉型和复脉带型等四种矿化类型金矿，具有一定的水平，垂直分带趋势和矿化地质特征．矿区围岩蚀变发育，蚀变分带因矿化类型不同，其发育程度各异，复合脉型金矿系矿区最重要的金矿类型，其蚀变分带模式，以含金石英脉为中心，向两侧依次为黄铁绢英岩化碎裂岩→黄铁绢英岩化黑云母花岗质碎裂岩→黄铁绢英岩化碎裂状黑云母花岗岩→碳酸盐化黑云母花岗岩→钾长石化黑云母花岗岩→黑云母花岗岩．蚀变作用期次可划分为成矿前钾长石化，成矿早期绢英岩化、绿泥石化、绿帘石化、成矿期硅化、黄铁矿化，成矿晚期碳酸盐化和高岭土化、与金矿化关系最密切者乃是硅化、黄铁矿化．
According to the arrangement of gold veins, structure of veins, production conditions, ore combination and construction, the veins can be divided into four types of mineralization: quartz vein type, altered rock type, complex vein type and complex vein type Types of gold ore, with a certain level, the trend of vertical zoning and mineralization geological features. The alteration and development of the surrounding rocks in the mining area is characterized by different mineralization types and different degrees of development. The most important type of gold deposit in the complex vein type gold deposit belongs to the alteration zoning mode, Center, to both sides of the yellow iron sericite metamorphic rocks → pyrite sericite biotite granitic crushed rocks → pyrite sericite fission-like biotite granite → carbonate biotite granite → potassium feldspar Biotite granite → biotite granite. The alteration period can be divided into pre-mineralization of K-feldspar, early mineralization of sericite, chlorite, epidote, silicification during mineralization, pyrite mineralization, later stage of carbonate mineralization and kaolin The most closely related to gold mineralization is silicification, pyrite mineralization.