摘要
介绍了金矿床围岩蚀变的概念,重点探讨了金矿床围岩蚀变特征,并对其地质意义进行分析,不仅可以更好的推断金属成矿物质的迁移、沉淀和富集机理,还可以阐明金矿床的矿床成因,为地质找矿工作的开展提供参考和借鉴,以期创造出更大的经济与社会效益。
In this paper,the concept of wall rock alteration in gold deposits is mainly introduced,and the alteration characteristics of the wall rocks in gold deposits are emphatically discussed and the geological significance is analyzed. This not only can better infer the migration and sedimentation of metallogenic minerals enrichment mechanism,but also elucidate the origin of gold deposits. It can provide reference and reference for the development of geological prospecting in order to create greater economic and social benefits.
引文
[1]周向科,王建国,易锦俊.云南冬瓜林金矿床的围岩蚀变特征和成矿阶段划分[J].中国矿业,2016,5(z1):45-46.
[2]张建胜,赵华林,张日德.胶北黑岚沟金矿床围岩蚀变特征及成因探讨[J].科技视界,2015,11(30):139-140.
[3]冯绍平,汪江河,刘耀文.熊耳山上宫金矿床围岩蚀变特征及找矿意义[J].矿产勘查,2017,6(3):86-87.