| 康古尔金矿地球化学分带模式及其预测标志 |
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| 引用本文： | 王磊.康古尔金矿地球化学分带模式及其预测标志[J].新疆地质,1993(4). |
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| 作者姓名： | 王磊 |
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| 作者单位： | 新疆维吾尔自治区地质矿产局第一地质大队 |
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| 摘 要： | 康古尔金矿受火山运动及韧性剪切作用双重控制;成矿母岩为中—酸性火山岩;矿化与黄铁绢英岩化、绿泥石化、硅化关系密切;指示元素组合类型,主要成矿元素Au和多金属为选择分布的两期成矿产物;矿床地球化学分带明显,但主要成矿元素相关性不明显,所建立的矿床剥蚀深度数学模式,对于矿脉勘探评价和寻找深部肓矿体具有一定的指导意义。
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| 关 键 词： | 康古尔金矿 地球化学 元素组合 相关系数 分带模式 新疆 |
GEOCHEMICAL ZONATION MODEL AND PREDICTION MARKS OF KANGUER GOLD DEPOSIT |
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| Wang Lei.GEOCHEMICAL ZONATION MODEL AND PREDICTION MARKS OF KANGUER GOLD DEPOSIT[J].Xinjiang Geology,1993(4). |
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| Authors: | Wang Lei |
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| Abstract: | The Kanguer gold deposit is controlled by volcanic activities and ductile shearing. Its mother rocks are intermediate-acid volcanics. The mineralization has a close relation with beresitization,chloritization and silicification. The indicative elements (association type) and the main ore-forming elements (Au and multi-metals) are the product of two different metallogenic stages. The geochemical zonation of the deposit is obvious,but that of the main ore-forming elements is not. A mathematic model of erosion depth is set up, which is significant to a certain extent on the prospecting and evaluation of ore veins and in the searching of deep blind ore bodies. |
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| Keywords: | Kanguer gold deposit geochemistry elements association correlation coefficient zonation model Xinjiang |
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