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新疆尼勒克县包尕斯达坂铜矿成矿模式探讨(增刊)
引用本文:南燕云,杨晓光.新疆尼勒克县包尕斯达坂铜矿成矿模式探讨(增刊)[J].中国矿业,2017,26(S1).
作者姓名:南燕云  杨晓光
作者单位:中国地质大学北京科学研究院,中国人民武装警察部队黄金第十支队
摘    要:包尕斯达坂铜矿床位于阿吾拉勒山西段,是尼勒克铜成矿带的重要组成部分。通过对矿床成矿地质背景、矿床地质、矿石特征及围岩蚀变的研究表明,该矿床为裂谷环境中火山热液充填形成的脉状矿床,不排除沉积过程中铜的初富集作用。

关 键 词:包尕斯达坂铜矿  矿床地质特征  矿床成因  成矿模式
收稿时间:2017/2/7 0:00:00
修稿时间:2017/5/15 0:00:00

Discussion on the Metallogenic Model of Baogasidaban Copper deposit in Nileke County, Xinjiang (Supplement)
Nan Yanyun and Yang Xiaoguang.Discussion on the Metallogenic Model of Baogasidaban Copper deposit in Nileke County, Xinjiang (Supplement)[J].China Mining Magazine,2017,26(S1).
Authors:Nan Yanyun and Yang Xiaoguang
Affiliation:Institute of Earth Sciences,China University of Geosciences,No.10 Detachment of General Gold Party/Chinese People ''s Armed Police Force
Abstract:The Baogasidaban copper deposit is located Western Awulale Mountain, Xinjiang, which is an important component of the Nileke copper-bearing belt. The study of ore-forming geological background, deposit geology, ore characteristics and wall rock alteration show that the Baogasidaban copper deposit is a vein type deposit formed by volcanic hydrothermal filling in the rift environmentthe, volcanic heat Liquid fill the formation of vein deposits, and does not exclude the initial enrichment of copper during the deposition process.
Keywords:Baogasidaban copper deposit  Geological characteristics of the deposit  Deposit genesis  Metallogenic model
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