贵州铜仁卜口场铅锌矿地质特征及成因  

Geological characteristics and genesis of the bokou field lead-zinc deposit in Tongren, Guizhou

作　　者：左丹 ZUO Dan(Guizhou geology and mineral exploration and Development Bureau 104 Geological Brigade.,Duyun 558000,China)

机构地区：[1]贵州省地矿地产勘查开发局一〇四地质大队,贵州都匀558000

出　　处：《世界有色金属》2018年第16期117-118,共2页World Nonferrous Metals

摘　　要：针对目前贵州铜仁卜口场对铅锌矿产资源的开发建设需求,文章分析了铅锌矿的地质特征,并总结了铅锌矿床的形成原因,其目的是提高铅锌矿产资源的开发建设效率。In view of the current demand for the development and construction of lead-zinc mineral resources in Tongrenbukouchang, Guizhou Province, this paper analyzes the geological characteristics of lead-zinc deposits and summarizes the causes of formation of lead-zinc deposits, aiming at improving the efficiency of development and construction of lead-zinc mineral resources.

关 键 词：贵州铜仁卜口场铅锌矿 沉积成矿 后期改造成矿 岩性控矿 

分 类 号：P618.43[天文地球—矿床学]