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现代矿业 ›› 2018, Vol. 34 ›› Issue (11): 35-40.

• 地质·测量 • 上一篇    下一篇

藏东母拉同铅锌矿地质特征及控矿因素

樊炳良1,冯德新1,白涛2   

  1. 1.西藏自治区地质矿产勘查开发局地热地质大队;2.成都理工大学地球科学学院
  • 出版日期:2018-11-25 发布日期:2018-12-27

Geological Characteristics and Ore-controlling Factors of Mulatong Pb-Zn Deposit,East Tibet

Fan Bingliang1,Feng Dexin1,Bai Tao2   

  1. 1.Geothermal Geological Survey Party,Tibet Bureau of Geology and Mineral Exploration and Development;2.College of Earth Sciences,Chengdu University of Technology)
  • Online:2018-11-25 Published:2018-12-27

摘要: 母拉同矿床大地构造位置处于班公湖—怒江蛇绿混杂岩带北东侧边界处,属三江成矿带中北段,区内成矿地质条件良好。分别从地层、构造、岩浆岩、1∶5万水系沉积物测量等方面总结了矿区成矿地质背景,分析了水系沉积物异常特征及岩石地球化学剖面特征,总结了矿床控矿因素。研究表明:①母拉同铅锌矿床具有良好的找矿潜力,区内NW向2组次级断裂破碎带的交汇部位为主要的容矿空间;②成矿有利地段具有明显的Ag、As、Cu、Pb、Sb、Sn等元素异常组合,且异常浓集中心较为突出;③成矿物质来源与超基性岩块无明显的成因联系,而与中酸性闪长玢岩脉存在成因关系;④硅化、褐铁矿化为矿区重要的间接找矿标志,地表铅锌矿(化)体露头、褐铁矿带为矿区的直接找矿标志;⑤矿石以侵染状、脉状为主,团块状、角砾状矿石主要分布于破碎带中。上述分析对于进一步在班公湖—怒江蛇绿混杂岩带东段寻找铜、铅、锌等有色金属矿产资源具有一定的参考价值。

关键词: 铅锌矿, 三江成矿带, 水系沉积物测量, 地质特征, 控矿因素, 找矿标志

Abstract: The tectonic position of Mulatong Deposit is located at the north eastern boundary of Bangong-Nujiang ophiolite belt,belonging to the northern part of Sanjiang Metallogenic Belt,and the metallogenic geological conditions are good in the area.The metallogenic geological background of the mining area is summarized from four aspects,such as strata,structure,magmatic rock,1∶50 000 stream sediment survey,and the anomalous characteristics of stream sediment survey and geochemical profile of the rocks are discussed,besides that,the ore-controlling factors are summarized.The study results show that:①Mulatong Pb-Zn Deposit has good prospecting potential,the intersection of the two groups of NW trending secondary faults in the area is the main ore-holding space;②favorable sections of the ore-forming zone has obvious abnormal combination of Ag,As,Cu,Pb,Sb,Sn and other elements,and the anomaly concentration center is more prominent;③there is no obvious genetic relation between the source of metallogenic materials ultrabasic rock blocks,but genetic relationship with the porphyrite dike and the source of metallogenic materials is existed;④silicification and ferritization are the important indirect prospecting indicators,and the Pb-Zn oremelt) outcrop and limonite ore belt in the surface of mining area are the direct prospecting indicators;⑤the ore shapes are mainly for invaded and veined,the ores with the shapes of crumby and breccia are mainly distributed in the fractured zone.The above study results related to Mulatong Pb-Zn Deposit can provide reliable reference for the further prospecting work of nonferrous metal mineral resources such as copper,lead and zinc in the east section of Bangong-Nujiang ophiolite belt.

Key words: Pb-Zn deposit, Sanjiang metallogenic belt, Stream sediment survey, Geological characteristics, Ore-controlling factor, Prospecting indicator