Abstract:

The Suolajier Cu-Mo deposit which was newly discovered in Qimantage in western part of eastern Kunlun Mountains, displays a geological feature of metals-bearing hydrotherm invading into broken skarn and marble. This paper summarizes its mineralization system through a mineralization process that Kunbei post-arc rift happened in early Paleozoic (Ordovician-Silurian), Tanjianshan formation from hot water sediment as the original mineral sources, the magma in Indosinian Epoch provided strong heat source and hydrotherm to reshape the skarn layer, metallic elements were enriched in broken skarn and marble into mineralization. This paper also discusses how to develop the deposit and studies the feasibility to establishing a mining town in Qinghua.

Key words: Suolajier Co-Mo deposit, mineralization system, stratified skarn, mining city

摘要：

东昆仑索拉吉尔铜钼矿床是近年新发现的一个矿床，其特征为含矿热液沿构造贯入矽卡岩和大理岩地层中成矿。笔者总结了索拉吉尔铜钼矿的成矿系统，认为昆北早古生代中期（奥陶—志留纪）弧后裂陷，热水沉积了滩间山群岩系，成为初始矿源层，印支期岩浆活动为该区带来了强大的热动力条件，热液交代作用重塑了层矽卡岩。成矿元素沿构造薄弱的破碎矽卡岩以及大理岩中发生矿化富集，叠加成矿。论文对该成矿带的开发进行了探讨，论述了在肯德可克建设矿城的充要条件。 

关键词: 索拉吉尔铜钼矿床, 成矿系统, 层矽卡岩, 矿业城市