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热液金矿床围岩蚀变特征及其与金矿化的关系
引用本文:黄诚,张德会,和成忠,等.热液金矿床围岩蚀变特征及其与金矿化的关系[J].物探与化探,2014(2):278-283,288.
作者姓名:黄诚  张德会  和成忠  
作者单位:[1]武警黄金第九支队,海南海口571127; [2]中国地质大学地球科学与资源学院,北京100083
摘    要:热液金矿床总是伴随着围岩蚀变,研究围岩蚀变对金矿勘查具有重要意义。总结不同类型热液金矿发现,与热液金矿密切相关的围岩蚀变主要有硅化、钾长石化、钠长石化、碳酸盐化、绿泥石化、绢英岩化等;重点分析讨论了硅化、钾长石化、钠长石化、碳酸盐化的特征、形成机理及其与金矿化之间密切关联的内在原因,同时也对热液金矿蚀变的分带性进行了讨论。

关 键 词:地球化学勘查  热液金矿床  围岩蚀变  蚀变分带

THE WALL-ROCK ALTERATION OF THE HYDROTHERMAL GOLD DEPOSIT AND ITS RELATIONSHIP WITH GOLD MINERALIZATION
Institution:HUANG Cheng, ZHANG Dehui, HE ChengZhong, WANG Xinyan, YU Xiao, Yin Haiyan ( 1.No.9 Gold Geological Party of CAPF,Haikou 571127, China; 2.School of Earth and Resources, China University of Geosciences,Beijing 100083, China )
Abstract:The hydrothermal gold deposit is always accompanied by wall rock alteration, which is of great significance for gold explora-tion. It is found that the wall rock alterations closely associated with the hydrothermal gold deposit include silicification, potassic altera-tion, albitization, carbonation, chloritization and propylitization, as shown by summary of different types of hydrothermal gold deposits. This paper has emphatically discussed the geochemical characteristics of silicification, potassic alteration, albitization, and carbonata-tion, and the reasons why gold mineralization is associated closely with these alterations. Alteration zoning of hydrothermal gold deposits is also briefly discussed.
Keywords:geochemical exploration  hydrothermal gold deposits  wall rock alteration  alteration zoning
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