| 黑龙江省争光金矿地质特征及成因初探 |
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| 引用本文： | 赵广江,侯玉树,王宝权.黑龙江省争光金矿地质特征及成因初探[J].有色矿冶,2006,22(3):3-6. |
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| 作者姓名： | 赵广江 侯玉树 王宝权 |
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| 作者单位： | 1. 中国地质大学,北京,100083;黑龙江省齐齐哈尔矿产勘查开发总院,黑龙江,齐齐哈尔,161006
2. 黑龙江省齐齐哈尔矿产勘查开发总院,黑龙江,齐齐哈尔,161006 |
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| 摘 要： | 争光金矿床产于中奥陶统多宝山组中性火山岩和燕山期中酸性侵入体中,赋存于NWW、NNW向断裂构造带内,矿体呈脉状,具有膨缩和尖灭再现特点.中奥陶统多宝山组中性火山岩地层为金矿之矿源层,燕山期中酸性侵入体岩浆作用为金矿的形成提供了热源,构造作用对含金热液的流动与迁移提供了通道.该金矿矿床成因为热液-构造蚀变岩型.
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| 关 键 词： | 争光金矿 地质特征 成因初探 黑龙江 |
| 文章编号： | 1007-967X(2006)03-0003-04 |
| 修稿时间： | 2005年10月27 |
Geological Characteristics and Genisis of Zhengguang Gold Deposit in Heilongjiang Province |
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| ZHAO Guang-jiang,HUO Yu-shu,WANG Bao-quan.Geological Characteristics and Genisis of Zhengguang Gold Deposit in Heilongjiang Province[J].Non-Ferrous Mining and Metallurgy,2006,22(3):3-6. |
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| Authors: | ZHAO Guang-jiang HUO Yu-shu WANG Bao-quan |
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| Abstract: | Zhengguang gold deposit is produced in Duobaoshan volcanism and Yanshan invasion,and occurs in NWW NNW tectonic belt.mineralization body occurs as vein type,and has the characteristics of dilatation,minimization,vanish and reappearance.Duobaoshan volcanism are source of gold mineralization belt;Yanshan invasion are hot source of gold mineralization.tectonic function provides road for gold-bearing thermal flow and transformation.The origin of this gold deposit is tectonic alteration type. |
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| Keywords: | Zhengguang gold deposit geological characteristics the origin of gold deposit Heilongjiang |
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