| 阿尔泰多金属成矿带矿床地质特征及其成矿历史演化 |
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| 引用本文： | 王少怀.阿尔泰多金属成矿带矿床地质特征及其成矿历史演化[J].地质找矿论丛,2006,21(2):80-86. |
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| 作者姓名： | 王少怀 |
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| 作者单位： | 中国地质科学院,矿产资源研究所,北京,100037;中国冶金地质勘查工程总局,第二地质勘查院,福建,莆田,351111 |
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| 基金项目： | 中国地质调查局区域地质调查项目 |
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| 摘 要： | 阿尔泰多金属矿带是世界上著名的铜-金-多金属成矿带,该带向东延伸至中国新疆北部阿尔泰地区,金、铜、多金属矿分布广泛.铜、多金属矿床产出受矿源层约束,海底火山喷流-沉积是最基本的成矿作用;金矿主要为火山热液型和与韧性剪切带有关的金矿类型.文章从矿床地质特征着手,分析它们的控矿条件和成矿历史的演化,探讨了金属矿床成因问题.
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| 关 键 词： | 阿尔泰 金-铜-多金属成矿带 矿床地质特征 成矿历史的演化 |
| 文章编号： | 1001-1412（2006）02-0080-07 |
| 收稿时间： | 2006-02-17 |
| 修稿时间： | 2006-04-12 |
MINERALIZATION EVOLUSION AND GEOLOGICAL FEATUERS OF ALTAY COPPER-GOLD POLYMETALLIC ORE BELT |
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| WANG Shao-huai.MINERALIZATION EVOLUSION AND GEOLOGICAL FEATUERS OF ALTAY COPPER-GOLD POLYMETALLIC ORE BELT[J].Contributions to Geology and Mineral Resources Research,2006,21(2):80-86. |
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| Authors: | WANG Shao-huai |
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| Institution: | 1. Institute of Mirteral Resources, CA GS,Beijing 100037 ,China; 2. No, 2 Geological and Exploration Institute of CEEB,Putian 351111, China |
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| Abstract: | Cu-Au polymetallic ore belt in Altay area,in the northern Xinjiang of China is famous in the world. Cu-Au polymetallic ore deposits are widely spreaded. Cu-Au polymetallic ore deposits are controled by source bed. SEDEX is a basic mineralizing process. The main gold ore deposit types are volcanic hydrothermal ore deposit and ductile shear-zone deposit. The paper analyzes the control factors and the evolution from the deposit features, then discuss their genesis. |
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| Keywords: | Altay Cu-Au polymetallic ore belt deposit feature metallogenic evolution |
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