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抱伦金矿床的赋矿层位为志留系下统陀烈组含碳千枚岩。豪岗岭“斜列式复背斜”控制矿床的空间展布。金矿体明显受北北西向相互平行的压扭性断裂形成的破碎带控制,金矿化与含矿石英脉中的不同期次形成的石英有关,其中以第二期为最主要的矿化期。矿区外围尖峰岭岩体至少由三期岩浆作用形成,与金矿床的形成有密切关系。金矿床成矿结束时期为217～221.2 Ma,属于印支晚期。抱伦金矿床属典型的受构造控制的含铋中温热液大—超大型金矿床。
The mineralization of the Baolun gold deposit is the Carboniferous phyllite from the Lower Ordovician Silurian. Ho Kong Ridge “Inclined Complex anticline ” control the spatial distribution of the deposit. The gold ore body is obviously controlled by the crushing zone formed by the compressive-torsional fractures that are parallel to each other in the north-northwest direction. Gold mineralization is related to quartz formed at different stages in ore-bearing quartz veins. The second phase is the most important mineralization period. The Jianfengling pluton outside the mining area is formed by at least three magmatism and is closely related to the gold deposit formation. The gold mineralization end of the period of 217 ~ 221.2 Ma, belonging to the late Indosinian. The Baolun gold deposit is a typical structural-controlled bismuth-bearing medium-temperature hydrothermal large-super-large gold deposit.