文章摘要
郎兴海.西藏自治区谢通门县斯弄多铅锌矿区地球物理特征及找矿方向[J].地质与勘探,2017,53(3):508-518
西藏自治区谢通门县斯弄多铅锌矿区地球物理特征及找矿方向
Geophysical characteristics and prospecting direction of the Sinongduo Pb-Zn deposit in Xietongmen county, Tibet
投稿时间:2016-11-08  修订日期:2016-12-03
DOI:10.12134/j.dzykt.2017.03.010
中文关键词: 斯弄多 激电中梯 林子宗群 低硫化型浅成低温热液型 地球物理 西藏
英文关键词: Sinongduo, induced polarization, Linzizong group, low-sulfidation epithermal deposits, geophysics, Tibet
基金项目:国家自然科学基金(编号:41172077,41502079)资助
作者单位E-mail
郎兴海 成都理工大学地球科学学院四川成都 中国地质科学院矿产资源研究所国土资源部成矿作用和资源评价重点实验室北京 西藏中瑞矿业发展有限责任公司西藏拉萨四川省冶金地质勘查局六〇五大队四川眉山 tangjuxing@126.com 
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中文摘要:
      浅成低温热液型矿床是一类主要产于陆相火山岩或与陆相火山岩有关的低温热液矿床,矿床埋藏深度浅是其最大的特点,这也使地球物理勘探方法在这类矿床的勘查中具有先天优势。本文通过对西藏斯弄多Pb-Zn-Ag多金属浅成低温热液型矿床的地球物理参数特征研究,采用激发极化法等综合物探技术在矿体外围探获具有巨大前景的Pb-Zn-Au-Ag浅成低温热液型矿体。目前单工程控制有3段矿体:顶部Au-Ag矿体,中部Au矿体,底部Pb-Zn-Ag矿体。矿体最高Au品味可达5.3g/t,Ag最高品味410g/t ,Pb+Zn综合平均品位5.9%。研究结果表明,斯弄多地区林子宗群火山岩物性参数稳定,对矿体异常干扰较小,产于该套火山岩中极强硅化体中的浅成低温热液型Au矿多具有中高极化率和中低阻特征。
英文摘要:
      The epithermal deposit is a kind of low-temperature hydrothermal deposits mainly hosted in continental volcanic rocks or related to continental volcanic rocks. The most important characteristic of this deposit is shallow burial depth, which makes geophysical methods have natural advantages in mineral exploration of epithermal deposits. Based on the study of geophysical characteristics of the Sinongduo polymetallic epithermal deposit, new Pb-Zn-Au-Ag epithermal hydrothermal orebodys are successfully discovered by using the integrated geophysical techniques such as the induced polarization. At present, there are 3 sections of ore bodies in the single project control, which are the top Au-Ag ore, the middle Au ore, and the bottom Pb-Zn-Ag ore. The highest grade of Au can reach 5.3 g / t and the Ag can be 410 g / t. The Pb+Zn grade is about 5.9 % on average. Research results show that the physical parameters of volcanic rocks of Linzizong group in the Sinongduo area are stable,and that the disturbance is relatively small. The Au epithermal deposits produced in the strongly silicified geologic masses of the Linzizong group volcanic rocks are mostly characterized by medium-high polarizability and medium-low resistance.
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