西藏甲玛铜多金属矿床是冈底斯成矿带东段与斑岩-夕卡岩成矿系统有密切联系的超大型铜多金属矿床。矿床以夕卡岩—斑岩型铜钼铅锌(金银)矿体为主,其现阶段工业开采以夕卡岩型铜多金属矿为主。矿区受区域构造影响较大,其形成的次一级断裂及褶皱横穿矿区,并控制着成矿岩体的产出状态。而当前关于甲玛矿床构造控矿方面的文献见之甚少,因此本文从构造因 The Jiama copper polymetallic deposit in Tibet is a very large Cu-polymetallic deposit closely linked with the porphyry-skarn metallogenic system in the eastern segment of the Gangdese metallogenic belt. The deposit is mainly composed of skarn-porphyry copper, molybdenum, lead-zinc (gold, silver) ore bodies, and industrial production at the current stage is dominated by skarn-type copper polymetallic deposits. The mining area is greatly affected by the regional tectonics. The secondary faults and folds formed across the mining area control the output status of the ore-forming rock mass. However, there is little literature on the ore-controlling aspects of the Jiama deposit. Therefore,