| 辽南隈子金矿成矿地质特征及成因讨论 |
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| 引用本文： | 彭省临,杨德江. 辽南隈子金矿成矿地质特征及成因讨论[J]. 岩土工程界, 1996, 0(3) |
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| 作者姓名： | 彭省临 杨德江 |
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| 作者单位： | 中南工业大学地质系，有色总公司辽宁地勘局研究所 |
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| 摘 要： | 隈子金矿床与辽河群盖县组合金硅质体关系密切，硅质体属于变质分异而成。矿床成因类型为变质—岩浆热液叠加改造型。矿床的形成过程可分为三大阶段：原始分散型矿源体阶段、变质再生型矿源体阶段、岩浆热液叠加改造型成矿阶段。辽南大多数金矿床的形成过程与隈子金矿相似。初步建立了这类与变质—岩浆作用有关的系列金矿床成矿模式。
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| 关 键 词： | 辽宁南部；成因类型；成矿模式；隈子金矿 |
THE CHARACTERISTICS AND GENESIS OF THE WEIZI GOLD DEPOSIT |
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| Peng Shenglin. THE CHARACTERISTICS AND GENESIS OF THE WEIZI GOLD DEPOSIT[J]. Geotechnical Engineering World, 1996, 0(3) |
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| Authors: | Peng Shenglin |
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| Abstract: | The Weizi gold deposit has close relation to An-bearing siliconite formed by metamorphic differentiation. It is genetically of metamorphic - magmatic hydrothermal superimposed one. The mineralization processis divided into three stages:formation of original source of dispersed ore materials, formation of metamorphic regenerated source and final mineralization by superimposation of magrnatic hydrothermal fluid. The metallogenic process of the most gold deposits in southern Liaoning is similar to that of the Weizi gold deposit. Our study was finalized at the establishment of metallogenic model of series gold deposits related to metarnorphism and magmatism. |
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| Keywords: | metallogenic process genetic type metallogenic model Weizi gold deposit |
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