| 阿尔泰山南缘赛都金矿床的构造-成矿流体及其演化 |
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| 引用本文： | 徐九华,张国瑞,谢玉玲,单立华,张绍俊,王平户,邹存海.阿尔泰山南缘赛都金矿床的构造-成矿流体及其演化[J].岩石矿物学杂志,2009,28(2):141-151. |
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| 作者姓名： | 徐九华 张国瑞 谢玉玲 单立华 张绍俊 王平户 邹存海 |
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| 作者单位： | 1. 北京科技大学,资源工程系,北京,100083
2. 新疆阿勒泰正元国际矿业公司,新疆,哈巴河,836700 |
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| 基金项目： | 国家自然科学基金，国家科技支撑计划 |
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| 摘 要： | 赛都金矿床位于新疆额尔齐斯构造带北西段,矿体受韧性剪切构造带的控制,赋存于玛尔卡库里巨型剪切带内的蚀变糜棱岩带内.构造-成矿流体早期以中高温、富CO2-N2等挥发分为特征,包裹体均一温度252.0～408.0℃;中期以CO2-H2O流体为主,包裹体均一温度203.0～325.8℃,反映了中温热液特征;中晚期演化为中低温、中低盐度的盐水溶液体系,包裹体均一温度120.0～221.0℃.矿石中黄铁矿的δ34S变化范围在3.53‰～5.88‰之间;铅同位素组成的206Pb/204Pb变化于18.099 7～18.358 5,207Pb/204Pb变化于15.487 7～15.579 0,208Pb/204Pb变化于38.111 6～38.355 1.硫铅同位素研究表明成矿物质是从深部富集的,在造山作用过程中从深部岩石通过热液萃取获得.主要的金矿化与后碰撞造山的伸展构造环境有关,构造-成矿流体的演化特征与剪切带演化过程相吻合.
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| 关 键 词： | 流体包裹体 成矿物质来源 赛都金矿 |
The evolution of tectonic metallogenic fluids in the Saidu gold deposit, Southern Altay |
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| XU Jiu-hu,ZHANG Guo-rui,XIE Yu-ling,SHAN Li-hu,ZHANG Shao-jun,WANG Ping-hu and ZHOU Cun-hai.The evolution of tectonic metallogenic fluids in the Saidu gold deposit, Southern Altay[J].Acta Petrologica Et Mineralogica,2009,28(2):141-151. |
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| Authors: | XU Jiu-hu ZHANG Guo-rui XIE Yu-ling SHAN Li-hu ZHANG Shao-jun WANG Ping-hu and ZHOU Cun-hai |
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| Institution: | Department of Resource Engineering, Beijing University of Science and Technology, Beijing 100083, China;Department of Resource Engineering, Beijing University of Science and Technology, Beijing 100083, China;Department of Resource Engineering, Beijing University of Science and Technology, Beijing 100083, China;Department of Resource Engineering, Beijing University of Science and Technology, Beijing 100083, China;Altay Zhengyuan International Mining Company, Habahe 836700, China;Altay Zhengyuan International Mining Company, Habahe 836700, China;Altay Zhengyuan International Mining Company, Habahe 836700, China |
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| Abstract: | |
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| Keywords: | fluid inclusions source of ore materials Saidu gold deposit |
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