摘要
江西省潭坑铅锌（银）矿区位于北武夷铅锌银成矿带内,本文系统阐述了矿区地质和矿床特征,并对矿床的成因进行了探讨。认为本区铅锌（银）矿床,经历了火山喷发沉积和后期热液充填两大成矿期,与次火山岩体（流纹斑岩）有密切的关系,属次火山热液矿床。
Tankeng lead-zinc（silver） deposit in Jiangxi province is located in the Northern WuyiMountain lead-zinc-silver metallogenic belt. This paper systematically describes geologicalsituation of mineralized area and characteristics of the deposit in order to discuss the gene-sis of the deposit. It is regarded that the deposit experienced two mineralization periods：volcanic-eruptive sedimentation and late hydrothermal filling. In addition, the deposit hasa close relationship with sub-volcanic rocks （rhyolite-porphyry） and belongs to the sub-volcanic hydrothermal deposit.
出处
《资源调查与环境》
2011年第1期29-36,共8页
Resources Survey & Environment
基金
江西永平地区矿产远景调查项目(矿调[2005]13-10号)资助
关键词
铅锌(银)
矿床特征
成因类型
喷发沉积
热液充填
次火山热液矿床
江西
lead-zinc （silver） deposit
characteristics of deposit
genetic types
erup-tive sedimentation
hydrothermal filling
sub-volcanic hydrothermal deposit
Jiangxi
