| 浅析广西某矿区多期岩浆侵入及成矿模式 |
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| 引用本文： | 杨宝丁,黄宇,李泽江. 浅析广西某矿区多期岩浆侵入及成矿模式[J]. 世界有色金属, 2020, 0(2): 229-229,231 |
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| 作者姓名： | 杨宝丁 黄宇 李泽江 |
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| 作者单位： | 广西壮族自治区地球物理勘察院 |
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| 摘 要： | 矿区位于属于南华淮地桂中-桂东台陷之大瑶山凸起,处于我国著名的钦杭成矿带中南部,成矿条件十分优越。矿区不同期次的岩浆侵入,控制着不同的矿床类型,各期次的岩浆侵入为本区带来了成矿物质来源和能量来源,北西向断裂则为区内主要的导矿构造和容矿构造。
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| 关 键 词： | 大瑶山隆起 钦杭成矿带 多金属矿 成矿模式 |
Analysis of multi-stage magmatic intrusion and metallogenic model in a mining area of Guangxi |
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| YANG Bao-ding,HUANG Yu,LI Ze-jiang. Analysis of multi-stage magmatic intrusion and metallogenic model in a mining area of Guangxi[J]. World Nonferrous Metals, 2020, 0(2): 229-229,231 |
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| Authors: | YANG Bao-ding HUANG Yu LI Ze-jiang |
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| Affiliation: | (Geophysical Survey Institute of Guangxi Zhuang Autonomous Region,Liuzhou 545005,China) |
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| Abstract: | The mining area is located in Dayaoshan uplift of Guizhong guidongtai depression in the South China Huaihe area,and in the south central part of qinhang metallogenic belt,which is famous in China.The metallogenic conditions are very good.The magmatic intrusions in different periods control different types of ore deposits.The magmatic intrusions in different periods bring the source of ore-forming materials and energy to the area.The NW trending faults are the main ore guiding and ore bearing structures in the area. |
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| Keywords: | Dayaoshan uplift qinhang metallogenic belt polymetallic ore metallogenic model |
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