| 果洛龙洼金矿床地质特征及成因探讨 |
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| 引用本文： | 文雪峰,伊有昌.果洛龙洼金矿床地质特征及成因探讨[J].中国工程科学,2005(4). |
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| 作者姓名： | 文雪峰 伊有昌 |
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| 作者单位： | 青海省有色地质矿产勘查局 西宁810007 |
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| 摘 要： | 果洛龙洼金矿床是近年在东昆仑造山带东段新发现的一处中型金矿床,通过对矿床的成矿地质条件、矿床地质特征,成矿机理的分析和研究,认为该矿床由早期形成的热水沉积建造提供主要成矿物质来源,在后期动力挤压、变形、变质作用下,成矿物质富集,形成含金石英脉型、构造蚀变岩型、具有典型的韧性剪切带型金矿床特点。
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| 关 键 词： | 果洛龙洼 金矿床 动力变质 韧性剪切带 |
Geological Characters and Genesis of Guoluolongwa Gold Deposit in Qinghai Province |
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| Wen Xuefeng,Yi Youchang.Geological Characters and Genesis of Guoluolongwa Gold Deposit in Qinghai Province[J].Engineering Science,2005(4). |
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| Authors: | Wen Xuefeng Yi Youchang |
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| Abstract: | Guoluolongwa gold deposit is a newly discovered middle deposit in Dongkunlun metallogenic belt.Based on analyses about geological characteristics, metallogenic mechanism of gold deposit,the gold deposit has been confirmed to be of quartz vein type and structural altered rock type. |
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| Keywords: | Guoluolongwa gold deposit geological characters genesis |
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