| 高龙金矿地质-地球化学特征及找矿意义 |
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| 引用本文： | 李存有.高龙金矿地质-地球化学特征及找矿意义[J].地质与资源,1994,3(4):278-288. |
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| 作者姓名： | 李存有 |
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| 作者单位： | 沈阳地质矿产研究所 |
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| 摘 要： | 研究表明：高龙隆起边缘的环状断裂为高龙金矿的控矿构造；成矿物质源于古生界碳酸盐岩和中生界砂泥岩；含矿热液为由雨水（含岩溶水）及岩浆水组成的深循环地下水；成矿环境为相对开放；金矿床为深循环地下水渗滤成因。总结归纳了高龙金矿成矿地质特征和地球化学特征，为便于寻找同类型矿床，提出了宏观和微观找矿标志。
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| 关 键 词： | 高龙金矿 地质-地球化学特征 成因探讨 找矿意义 |
| 收稿时间： | 1994-03-14 |
THE GEOLOGICAL AND GEOCHEMICAL FEATURES OF GAOLONG GOLD DEPOSIT AND THEIR SIGNIFICANCE IN GOLD SEARCHING |
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| Li Cunyou.THE GEOLOGICAL AND GEOCHEMICAL FEATURES OF GAOLONG GOLD DEPOSIT AND THEIR SIGNIFICANCE IN GOLD SEARCHING[J].Geology and Resources,1994,3(4):278-288. |
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| Authors: | Li Cunyou |
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| Institution: | Shenyang Institute of Geolegy and Mineral Resources |
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| Abstract: | Abstract Gaolong gold deposit is a typical impregnation gold deposit in northwestern GuangXi· Inorder to search GaoLong type gold deposit in this area， this paper studied the geological andgeochemical diaracte─ristics of Gaolong gold deposit and came to this conclusion ： the ringfault around the GaoLong swell is the gold minerogenetic control fault； some of metallo-genitic element came from the wall─rock （Trias arenaceous─pelitic rock and Permian Sys-tem carbonatite）；the gold hydrothermal is the circulation subsurface vvater that is made fromrain （include karst water）and magmatic water； the minerogenetic environment was open andGaoLong gold deposit is hypogene circulation subsurface water infiItration type in gene-sis。 Finally，this paper summarized the geological and geochemicel symbols in gold searching. |
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