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九瑞铜多金属矿集区是长江中下游铁铜多金属成矿带的重要组成部分,区内主要矿床类型包括:与燕山期钙碱性富钾富硅壳幔混源中-酸性侵入体(石英闪长玢岩、花岗闪长斑岩和石英斑岩)有关的斑岩型、矽卡岩型Cu-Mo-Au矿床以及赋存于上石炭统黄龙组底部的层状硫化物型Cu-S-Au-Ag-Pb-Zn矿床,斑岩型矿床如城门山、丁家山、洋鸡山、宝山、丫头山等,矽卡岩型矿床如武山、城门山、邓家山、东雷湾等,
The Jiurui copper polymetallic ore deposit is an important part of the iron-copper polymetallic metallogenic belt in the middle and lower reaches of the Yangtze River. The main deposit types in the area include: medium-acidic intrusive (Quartz diorite porphyrite, granodiorite porphyry and quartz porphyry) porphyry-type and skarn-type Cu-Mo-Au deposits as well as the layered sulphide type hosted in the bottom of the Upper Carboniferous Huanglong Formation Cu-S-Au-Ag-Pb-Zn deposits and porphyry deposits such as Chengmenshan, Dingjiashan, Yangjishan, Baoshan and Yaoshan, skarn deposits such as Wushan, Chengmenshan, Dengjiashan, East Thunder Bay and so on,