渣滓溪锑(钨)矿区位于区域性北东向主干断裂F1、F2及矿区南西侧北西向F3断裂所夹持的上升地块内.构造在矿床形成过程中起到了极其重要的作用,区域性北东向主干断裂控制着次级F3断裂,起导矿作用;F3上盘的更次级断裂为容矿构造,是良好的储矿场所;F3断裂为配矿构造,起联通导矿和容矿构造的作用.研究矿区构造控矿特征,对矿区深边部找矿、勘探及采矿具有十分重要的意义.
@@@@Zhazixi antimony(tungsten) deposit is located in the elevated block between the regional main faults F1 ,F2 trending northeast and the northwest trending fault F 3 southwest to the deposit.Structure plays a very important part in ore formation process.The regional main faults control the secondary fault F 3 ,acting as ore-transmitting struc-ture.Secondary fault of the hanging wall of F 3 is an ore-hosting structure.F3 fault is an ore-blending structure,acting as the connection of ore-transmitting and ore-hosting structures.It would be very helpful for the deep and extensional prospecting,exploration and mining in the deposit to study the structural ore-controlling characteristics.
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