| 清原花岗—绿岩区金矿地质特征及矿床成因研究 |
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| 引用本文： | 卞伟国 张玉华. 清原花岗—绿岩区金矿地质特征及矿床成因研究[J]. 黄金, 1991, 12(2): 1-6 |
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| 作者姓名： | 卞伟国 张玉华 |
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| 作者单位： | 中国有色金属工业总公司吉林矿产地质研究所(卞伟国)，国家黄金管理局长春黄金研究所(张玉华) |
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| 摘 要： | 清原地区是一个花岗——绿岩区,绿岩是在晚太古代年轻地体裂谷期形成。该区的金矿床基本是在绿岩带形成之后由不同的地质作用形成的,共分四种成因类型。该区是个金矿集中区,也是一个金矿找矿的重要靶区。
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| 关 键 词： | 花岗－绿岩区 金矿床 成因 |
Study on geological characteristics and genesis of gold deposit in Qing-Yuan granite-greenstone terrain |
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| Bian Weiguo Zhang yuhua. Study on geological characteristics and genesis of gold deposit in Qing-Yuan granite-greenstone terrain[J]. Gold, 1991, 12(2): 1-6 |
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| Authors: | Bian Weiguo Zhang yuhua |
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| Affiliation: | Jilin Institute of Minereal Resources and Geology CNNC and Changchun Gold Research Institute |
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| Abstract: | Qing-Yuan district is a granite-greenstone terrain, The greenstone was formed during the youth stage of massif rifting in late Archean. Gold deposits were occurred by the various geological functions after greenstone belt formed. The genesis of gold deposit can de divided into four types.This district is a concentrated area of gold deposit and an important target for gold prospecting |
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| Keywords: | granite-greenstone terrain genetic type of gold deposit meta-morphic hydrothermal ductile shear zone magmatism of activation. |
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