| 陆品义.高村金矿床11-1矿体富矿段地质特征及成因[J].地质找矿论丛,2002,(2):92-96 |
| 高村金矿床11-1矿体富矿段地质特征及成因 |
| THE GEOLOGICAL CHARACTERISTICS AND ORIGIN OF THE RICH ORE SEGMENT IN 11-1 ORE BODY, GAOCUN Au DEPOSIT |
| 投稿时间：2002-01-04 修订日期：2002-04-15 |
| DOI：10.6053/j.issn.1001-1412.2002.2. 004 |
| 中文关键词: 河台金矿 富矿段 韧性剪切带 重熔花岗岩 成矿热液 小矿体 广东省 |
| 英文关键词:rich ore segment ductile shear zone remelting granite mineralizing thermal fluid minor ore body Hetai Au deposit Guangdong |
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| 中文摘要: |
| 通过对河台金矿高村矿床11-1矿体富矿段的富集特征及赋存状况的研究,分析了富矿段的形成与构造、重熔花岗岩、成矿热液之间的关系,阐明了富矿段的成因及经济意义,同时指出与主矿体平行侧列的小矿体的探矿方向。 |
| 英文摘要: |
| Studying of the enrichment characteristics and occurrence of the rich ore segment in 11-1 Ore Body Gaocun Deposit, Hetai Gold Mine, and analysis of the origin and structure of the rich ore segment as well as its' relation with remelting granite and ore fluid imply ore formation and economical importance of the rich ore segment. And the ore-search direction of minor ore body paralleled with major ore body is also indicated. |
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