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卡林型金矿床主要产于狭义扬子地块周边的古生代、中生代坳陷区内，即稳定地块与活动地块之间的构造过渡带。明显受构造控制，具有分级控制特点，区域性深大断裂控制着金矿带的分带，旁侧次级断裂，短轴背料或穹隆控制着矿床，更低序次断裂控制着矿体的定位。
Carlin-type gold deposits are mainly produced in the Paleozoic and Mesozoic depression areas around the narrow Yangtze block, namely, the structural transitional zone between the stable block and the active block. It is clearly controlled by tectonics and has the characteristics of grading control. The regional deep faults control the zoning of the gold belt, the secondary side faults, the short axis back material or the dome control the ore deposit, and the lower order faults control the ore body Positioning.