| 木梓园钨钼矿床流体包裹体研究及在成矿阶段划分中的应用 |
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| 引用本文： | 刘若兰,慕纪录.木梓园钨钼矿床流体包裹体研究及在成矿阶段划分中的应用[J].成都理工大学学报(自然科学版),1990(3). |
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| 作者姓名： | 刘若兰 慕纪录 |
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| 作者单位： | 成都地质学院地质矿产勘查系
(刘若兰)，成都地质学院地质矿产勘查系(慕纪录) |
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| 摘 要： | 通过对江西木梓园钨钼矿床中流体包裹体的研究。认为该矿床是在高一中温、中低盐度、碱性成矿溶液、弱还原条件下形成的。矿质主要来源于岩浆热液。成矿具脉动特征,可分为4个成矿阶段。
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| 关 键 词： | 流体包裹体 均一温度 气相百分数 还原参数 成矿阶段 围岩蚀变 |
RESEARCH ON FLUID INCLUSIONS AND ITS APPLICATION TO THE STUDY OF OREFORMING STAGES IN THE MUZIYUAN W-Mo DEPOSIT, JIANGXI PROVINCE |
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| Liu Ruolan,Mu Jilu.RESEARCH ON FLUID INCLUSIONS AND ITS APPLICATION TO THE STUDY OF OREFORMING STAGES IN THE MUZIYUAN W-Mo DEPOSIT, JIANGXI PROVINCE[J].Journal of Chengdu University of Technology: Sci & Technol Ed,1990(3). |
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| Authors: | Liu Ruolan Mu Jilu |
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| Institution: | Liu Ruolan;Mu Jilu |
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| Abstract: | According to fluid inclusion research, it is suggested that the Muriyuan W-Modeposit was formed weakly reducing and alkaline hydrothermal solutions with medium-lowsalinities and under high-mcdium tempcratures. The ore-forming solutions and theircontents were probably of magmatic origin. The ore-forming process was characterized byintermittence. And four ore-forming stages are recognized. |
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| Keywords: | fluid inclusion homogenization temperature liquid/vapour ratio reducing parameter ore-forming stage wall-rock alteration |
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