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甲玛铜多金属矿位于冈底斯成矿带东段,是与中新世构造-岩浆活动有关的铜、钼、铅、锌、金、银、钨、锡成矿亚系列中的典型代表,随着勘探及研究的不断深入,甲玛铜多金属矿成矿模式日益完善,形成了斑岩-夕卡岩-角岩型三位一体的成矿模型(唐菊兴等,2010;郑文宝等,2010)。矿床
The Jiama copper polymetallic deposit is located in the eastern segment of the Gangdese metallogenic belt and is a typical representative of the sub-series of copper, molybdenum, lead, zinc, gold, silver, tungsten and tin mineralization associated with the Miocene tectono-magmatic activities , With the deepening of exploration and research, the metallogenic model of the Jiama copper polymetallic deposit has been increasingly improved, forming a porphyry-skarn-hornstone trinity metallogenic model (Tang Juxing et al., 2010; Zheng Wenbao et al., 2010) . Deposits