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投稿时间：2015-12-21 修订日期：2016-11-04
投稿时间：2015-12-21 修订日期：2016-11-04
中文摘要: 对云南九顶山斑岩铜钼矿含矿石英脉中的石英流体包裹体分析表明,九顶山铜钼矿成矿流体属于NaCl-H2O型,均一温度集中在260~320℃,盐度集中在6.50~10.60%,成矿流体为中低温、中等盐度性质；流体包裹体压力及深度分析显示,成矿流体主要在低压环境下形成,流体演化过程中压力逐渐释放,深度逐渐降低。
Abstract:The ore-forming fluid of the Jiudingshan porphyry Cu-Mo deposits is the NaCl-H2O system based on research of Characteristics of the Fluid Inclusion and the ore-forming is characterized by low temperature and lower salinity. The temperature concentrated between 260℃ and 320℃ and the salinity concentrated between 6.50% and 10.60%. Pressure and depth analysis shows that Ore-forming fluid mainly formed in low pressure shallow-seated environment, the pressure and depth were gradually reduced with fluid evolution.
文章编号： 中图分类号：P618.41；P618.65 文献标志码：
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引用文本：
陆世才,李峰,刀艳.云南九顶山斑岩铜钼矿流体包裹体特征及地质意义[J].有色金属工程,2016,6(6):92-95.
陆世才,李峰,刀艳.云南九顶山斑岩铜钼矿流体包裹体特征及地质意义[J].有色金属工程,2016,6(6):92-95.
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