摘要
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 F3 southwest to the deposit.Structure plays a very important part in ore formation process.The regional main faults control the secondary fault F3,acting as ore-transmitting structure.Secondary fault of the hanging wall of F3 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.
出处
《黄金》
CAS
2013年第5期23-26,共4页
Gold
关键词
渣滓溪锑(钨)矿区
区域构造
矿区构造
构造控矿
Zhazixi antimony（tungsten） mining area
regional structures
structures in mining area
structural ore control
