新疆蒙马拉铅锌矿床地质特征及成因分析  

The geological characteristics and explananon of the Mengmala lead-zinc deposit, Xinjiang

作　　者：彭戈[1] 王子龙[1] 王勇[1,2] 赵玉梅[3] 

机构地区：[1]成都理工大学,四川成都610059 [2]中国地质调查局成都地质调查中心,四川成都610081 [3]新疆地质矿产勘查开发局第七地质大队,新疆乌苏833000

出　　处：《世界有色金属》2016年第5期112-113,共2页World Nonferrous Metals

摘　　要：蒙马拉铅锌矿区位于新疆尼勒克县蒙马拉林场一带，处于博罗霍洛古生代复合岛弧带中段，赋矿地层为下石炭统大哈拉军山组（C，d），蒙马拉铅锌矿产于该组的火山角砾岩a-#k＆触矽卡岩中。由于本区前人研究程度不足，笔者结合前人资料，以地质队项目为依托，对矿区矿床地质特征、成因类型及找矿标志进行系统研究总结，补充本区研究资料，以期对同类矿床找矿及提供一定的指导。The Mengmala lead-zinc deposit was located in Nileke County, Xinjiang Province, Mengmala forest area. In the central part of the Boluohuoluo arc belt. The lead-zinc mine were mainly hosted in the Lower Carboniferous Dahalajunshan Formation （Cld） and out of volcanic breccia and outer contact skarn. In this area, the research degree is not enough. On the basis of the combination of previous data, this paper relies on the geological team projects. Writer has systematic research and summing-up the deposit geological characteristics, genetic type and ore prospecting indicators. Supplement the research information of this area. In order to provide some guidance for find similar ore deposit.

关 键 词：蒙马拉 铅锌矿 接触交代 矽卡岩 

分 类 号：TD854.6[矿业工程—金属矿开采]