| 内蒙古大黑山金矿成矿物理化学环境 |
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| 引用本文： | 张丽娟,王晓勇. 内蒙古大黑山金矿成矿物理化学环境[J]. 材料与冶金学报, 2001, 0(2) |
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| 作者姓名： | 张丽娟 王晓勇 |
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| 作者单位： | 武警黄金第六支队(张丽娟)，武警黄金第六支队(王晓勇) |
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| 摘 要： | 通过对大黑山金矿床的基本特征、金矿床的流体包裹体和硫、铅、氢氧同位素特征研究分析 ,认为该矿床形成在一种中温浅成的环境下 ,成矿溶液具有富含H2 O ,CO2 ,SO2 -4 和高Na+ 的特点 ,是岩浆热液和变质水的混合流体 ,成矿物质主要由深源岩浆提供
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| 关 键 词： | 金矿床 成矿溶液 流体包裹体 稳定同位素 内蒙古 |
Study on the Conditions of Metallogenetic Physical Chemistry ln Daheishan Gold Deposit, lnner Mongolia |
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| Zhang Li juan Wang Xiao yong. Study on the Conditions of Metallogenetic Physical Chemistry ln Daheishan Gold Deposit, lnner Mongolia[J]. Journal of Materials and Metallurgy, 2001, 0(2) |
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| Authors: | Zhang Li juan Wang Xiao yong |
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| Affiliation: | Zhang Li juan Wang Xiao yong |
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| Abstract: | The basic features of Daheishan gold deposit are introduced in this paper, According to the analysing fluid inslusion, S,Pb,H and O isotopes, it is considered that the gold deposit was formed in a moderate temperature and shallow depth condition. The ore forming fluid have features of rich H 2O,CO 2,SO 2- 4 and high Na +, it is the mixture of magmatic water and metamorphic water. The mineralizing mass are mainly provided by plutonic magma. |
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| Keywords: | gold deposit ore forming fluid fluid inslusion stable isotope Inner Mougolia. |
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