东昆仑索拉吉尔铜钼矿床成矿系统及开发条件  

MINERALIZATION SYSTEM AND DEVELOPMENT CONDITIONS OF SUOLAJIER CU-MO DEPOSIT IN EASTERN KUNLUN

作　　者：刘正荣 杨永强[2] 李钟山[3,4] 陈兴华[4] 王斯林 张世勤 

机构地区：[1]新疆地质矿产局物化探大队,新疆昌吉831100 [2]中国地质大学地质过程与矿产资源国家重点实验室,北京100083 [3]北京大学地球与空间科学学院,北京100871 [4]国土资源部中央地质勘查基金管理中心,北京100045 [5]青海省胜华矿业有限责任公司,青海格尔木816000

出　　处：《资源与产业》2010年第4期129-132,共4页Resources & Industries

基　　金：中国地质大学地质过程与矿产资源国家重点实验室开放课题(GPMR200624);新疆物化探大队项目(KY02)

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。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.

关 键 词：索拉吉尔铜钼矿床 成矿系统 层矽卡岩 矿业城市 

分 类 号：P618.41[天文地球—矿床学]