CAJ | 학술논문

本文简要介绍了咸康矿区铅锌多金属矿的成矿地质背景和矿床地质特征，并分析了成矿与地层、岩浆岩、构造三者间的关系。即矽卡岩岩层提供赋矿层位，岩浆热液提供成矿物质、热源、水源和动力，层间裂隙提供储矿空间，东西向断裂提供导矿通道。从而认为本矿床为一矽卡岩型多金属矿床。
본문간요개소료함강광구연자다금속광적성광지질배경화광상지질특정，병분석료성광여지층、암장암、구조삼자간적관계。즉석잡암암층제공부광층위，암장열액제공성광물질、열원、수원화동력，층간렬극제공저광공간，동서향단렬제공도광통도。종이인위본광상위일석잡암형다금속광상。
This paper describes briefly the geologic setting and ge-ological characteristics of the Xiankang Pb-Zn polymetallic ore de-posit, discovers that the orebodies are situated in bedding fissure of skarn and controlled by EW-trending transversal faults.Magmatic fluid brought an abundance of mineral elements and afforded dynamic force. By analysis of the ore-forming relationship with strata,magmatite and structure,it is suggested that the Xiankang deposit is a polymetallic skarn deposit.