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燕山地区中元古界碎屑岩—碳酸盐岩系内赋存着似层状金矿、古砾岩型金矿、似层状银多金属矿、层状铅锌矿、夕卡岩型铜多金属矿及火山岩型铜矿６种不同类型的矿床。古砾岩型金矿、火山岩型铜矿与层状铅锌矿分别形成于中元古宙常州沟期、大红峪期与高于庄期；似层状金矿、银多金属矿与夕卡岩型铜多金属矿则主要形成于中生代燕山期。中元古宙金多金属矿化的空间分布受同沉积构造、岩相古地理与古沉积环境等因素所制约，而燕山期金、银、多金属矿化的空间分布主要受中元古界地层层序与燕山期构造—岩浆活动所控制。
In the Middle Paleoproterozoic clastic-carbonate rocks in the Yanshan area, stratiform gold deposits, ancient conglomerate-type gold deposits, stratified silver polymetallic deposits, stratiform lead-zinc deposits, skarn-type Copper polymetallic ore and volcanic copper deposits of 6 different types of deposits. The ancient conglomerate-type gold deposits, volcanic-type copper deposits and layered lead-zinc deposits were formed in the Middle Proterozoic Changzhou gully period, Dahongyu period and higher period than the Zhuang period; similar to the layered gold deposit, silver polymetallic deposit, Rock type copper polymetallic deposits are mainly formed in the Mesozoic Yanshan period. The spatial distribution of gold polymetallic mineralization in the Mesozoic Archean was controlled by the synsedimentary structure, lithofacies paleogeography and paleo-sedimentary environment. The spatial distribution of gold, silver and polymetallic mineralization in the Yanshan Period was mainly affected by the Proterozoic Stratigraphic sequence and Yanshanian tectono-magmatic activity.