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西藏甲马铜多金属矿床的成因前人已提出了很多种观点。根据野外地质特征的观察 ,并结合矿区和区域岩矿石的微量元素、常量元素和稀土元素的分析与对比 ,作者认为该矿床的成因属于岩浆热液交代矽卡岩型矿床 ,推测其成矿时代为喜山早期。
The origin of the Tibet Jiama copper-polymetallic deposit has been proposed by many people. Based on the analysis of field geologic features and the analysis and comparison of trace elements, major elements and rare earth elements in rock ore areas and areas, the authors believe that the genesis of the deposit belonged to the magmatic hydrothermal metasomatolite skarn deposit and speculated that the mineralization age Himalayan early.