| 东昆仑哈拉郭勒金矿地质特征及成因初探 |
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| 引用本文： | 彭涛,蔺思佳.东昆仑哈拉郭勒金矿地质特征及成因初探[J].甘肃冶金,2017,9(1):56-59. |
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| 作者姓名： | 彭涛 蔺思佳 |
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| 作者单位： | 1. 青海省有色地勘局矿勘院,青海 西宁,810000;2. 青海省地方铁路投资有限公司,青海西宁,810000 |
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| 摘 要： | 哈拉郭勒金矿位于布尔汗布达山华力西一印支期钴、金、铜、玉石成矿带,为热液蚀变岩型金矿。金矿体呈脉状,分布于石炭系地层的控矿构造中,具有强烈的围岩蚀变。通过对该区金矿地质特征进行分析,对矿体成因进行初步的探讨。
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| 关 键 词： | 哈拉郭勒金矿 热液蚀变岩型金矿 围岩蚀变 成因探讨 |
Geologic Feature and Genesis of Halaguole Gold Deposit,East Kunlun |
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| PENG Tao,LIN Si-jia.Geologic Feature and Genesis of Halaguole Gold Deposit,East Kunlun[J].Gansu Metallurgy,2017,9(1):56-59. |
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| Authors: | PENG Tao LIN Si-jia |
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| Abstract: | Halaguole gold deposit is located in burhan budai mountains of the Variscan-Indosinian cobalt, gold, copper, jade metallogenic belt ,it is hydrothermal altered rock type gold deposit.Gold orebodies are vein, In the ore controlling structure of carboniferous strata,with strong wall rock alteration.Based on the analysis of the geological features of the gold deposits in this area, the origin of the ore bodies is preliminarily discussed. |
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| Keywords: | Halaguole gold hydrothermal altered rock type gold deposit wall rock alteration discussion on origin |
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