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倒木河金矿为吉林中部矿化集中区中主要矿床。区域大地构造环境决定了矿化集中区的成矿地质条件和区域成矿系列的产出。区域上北东向小城子—口前，双河镇—西阳两条左行剪切断裂和小城子—双河镇北西向断裂为导岩、导矿构造，控制该矿床的产出。两条北东向左行剪切断裂产生的次级裂隙构造控制矿体和矿脉的产出，为矿床的容矿构造。从该区所具有的区域构造环境至区域控矿断裂构造到次级容矿裂隙构造，构成了三级控矿系统。控矿断裂和裂隙构造受统一的不同序次的构造应力场作用所致。
The inverted wood river gold mineralization in central Jilin Province as the main deposit. The terrestrial tectonic environment determines the mineralization geological conditions and the regional metallogenic series output. In the area, two left-lateral shear faults from the north-east to the front of the mouth-Shuanghe-Xiyang and the north-west fault of Xiaochengzi-Shuanghe are dominated by rock and ore-bearing structures and controlled the output of this deposit. The secondary fissures formed by the two NE-I left shear faults control the ore body and vein output, which is the ore-hosting structure of the deposit. From the regional tectonic environment in this area to the regional ore-control fault structure to the secondary ore-bearing fracture structure, a tertiary ore control system is formed. The ore-controlling faults and fissures are affected by the unified structural stress fields of different orders.