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烧锅营子地区金矿的形成主要是由构造活动、岩浆侵入和围岩蚀变等成矿控制因素综合作用的结果，东西向构造带严格控制着金矿带、金矿床呈等距离展布，与其具有成生联系的次级东西向、北东向和北西向断裂又是含金矿脉的主要容矿构造．合金矿脉皆产于岩体边缘相地带，且与细粒闪长岩脉相伴而存，表明脉岩矿脉于空间上、时间上及成因上和燕山期黑云母花岗岩浆的演化活动有关，三者为同源关系．
The formation of the gold deposits in the Xiaogouyingzi area is mainly caused by the combined effects of tectonic activities, magma intrusion and alteration of surrounding rocks and other metallogenic factors. The gold belts are strictly controlled by the east-west structural belt and the gold deposits are equidistantly distributed. Its secondary east-west, north-east and northwest faults, which are closely related to each other, are the main ore-bearing structures of gold-bearing veins. The alloy veins are all produced in the marginal zone of the rock body and are accompanied by fine diorite veins, indicating that the veins of veins are related to the evolution of the Yanshanian biotite granite magma in space, time and genesis. The three Homologous relationship.