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五龙金矿床为辽东南地区一大型典型石英脉型金矿床,它产于印支期黑云母花岗片麻岩之中,矿脉的产出严格受断裂构造控制.在前人研究工作基础上,结合多年来矿山地质工作实践,系统总结了矿区断裂构造控矿规律,分析和总结了进一步找矿地质标志,这对矿区生产探矿工作有重要指导意义.

Wulong gold deposit is a large-scale, typical quartz vein type gold deposit in southeastern Liaoning province. It occurred in biotite granitic gneiss of Indo-Chinese epoch and the occurences of gold veins were strictly controlled by faults. On the base of previous studies and long years' geological practice in the gold mine, the fault structure-controlling regularities of gold mineralization were summed up and the geological marks for subsequent pros-pecting were analyzed. The study was of great signicances to the production and prospecting in Wulong gold mine.

参考文献

[1] 魏俊浩,刘丛强,唐红峰.辽东五龙地区燕山期侵入岩类同源岩浆演化微量元素、同位素证据与金矿成矿[J].地质论评,2003(03):265-271.
[2] 杨春福 .辽宁五龙金矿床容矿断裂构造与金矿体空间赋存特征[J].黄金,1997,18(03):3-8.
[3] 吕贻峰,李江风.辽宁丹东五龙金矿矿化类型及其构造控制机理[J].现代地质,1994(03):309.
[4] 彭艳东 .五龙金矿成因研究[J].贵金属地质,1994,3(01):21-31.
[5] 肖国洪,刘铁侠,张国宪.辽宁五龙金矿床成因与成矿模式探讨[J].黄金,2003(11):17-21.
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