| 湘南东坡矿田钨锡成矿系列流体同位素特征 |
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| 引用本文： | 崔彬,赵磊.湘南东坡矿田钨锡成矿系列流体同位素特征[J].矿物岩石地球化学通报,2001,20(4):328-330. |
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| 作者姓名： | 崔彬 赵磊 |
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| 作者单位： | 中国地质大学,北京,1000833 |
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| 摘 要： | 东坡矿田是华南成矿区的重要组成部分 ,区内不同的含矿岩浆岩叠加于不同类型的含矿建造之上 ,形成了不同类型的矿床和W、Sn成矿系列。从早到晚 ,含矿流体从富岩浆水→富大气降水 ,伴随这一演化趋势 ,主成矿元素从W、Sn→Sn、Cu→Pb、Zn。从而形成了东坡矿田W Sn成矿系列。
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| 关 键 词： | 东坡矿田 成矿系列 流体 同位素 |
| 文章编号： | 1007-2802(2001)04-0328-03 |
| 修稿时间： | 2001年6月11日 |
Fluid Isotope Characteristics of the W-Sn Metallogenic Series in Dongpo Ore Field, South Hunan Province |
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| CUI Bin,ZHAO Lei.Fluid Isotope Characteristics of the W-Sn Metallogenic Series in Dongpo Ore Field, South Hunan Province[J].Bulletin of Mineralogy Petrology and Geochemistry,2001,20(4):328-330. |
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| Authors: | CUI Bin ZHAO Lei |
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| Abstract: | Dongpo ore field is an important part of Hunan metallogenetic area. In the area, different ore-bearing magma were superimposed over different ore-formation, and came into being various types of deposits and W-Sn metallogenic series.From early time to late time , the fluid changed from magmatic water to richness in atmospheric water. With the variation of this evolution, the main ore-forming elements change from W, Sn to Sn, Cu and eventually to Pb, Zn. Therefor W,Sn metallogenic series is formed in the Dongpo ore field. |
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| Keywords: | Dongpo ore field metallogenic series fluid isotope |
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