| 新疆西准噶尔齐Ⅰ金矿氧、硫、氢、碳同位素特征及成矿机理探讨 |
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| 引用本文： | 刘绍忠.新疆西准噶尔齐Ⅰ金矿氧、硫、氢、碳同位素特征及成矿机理探讨[J].新疆地质,1990(1). |
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| 作者姓名： | 刘绍忠 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第七地质大队 |
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| 摘 要： | 系统的地球化学研究结果确定了齐Ⅰ号矿区的成矿元素来自岩浆岩,金主要以S、Cl络合物形式迁移,确定了金沉淀的最佳温度、PH值、fO_2,氧化还原条件,认为该金矿为中深成矿床.
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| 关 键 词： | 新疆齐Ⅰ金矿 同位素 包裹体 物理化学特征 成矿机理 |
O.S.H.C. ISOTOPE GEOCHEMISTRY AND MINEROGENESIS OF 01-1 GOLD DEPOSIT,JUNGGAR,XINJIANG |
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| Liu Shaozhong.O.S.H.C. ISOTOPE GEOCHEMISTRY AND MINEROGENESIS OF 01-1 GOLD DEPOSIT,JUNGGAR,XINJIANG[J].Xinjiang Geology,1990(1). |
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| Authors: | Liu Shaozhong |
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| Abstract: | Systematic study of O.S.H.C isotopes shows that the minerogenetic elememts of Qi-1 gold deposit originated from the magmatic rocks. Au can be migrated mainly in the ways of S.C1 complex. The author considers that the Qi-1 gold deposit was formed in the middll depth. And the optimun temperature, pH, fO2 and the condition of Oxidation-Reduction during precipitation of gold are presented in this paper. |
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| Keywords: | Qi-1 gold deposit in Xinjiang isotope inclusios physicochemical characteristic mineralizing mechanism |
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