摘要
黄柏坑铅锌(铜银)矿区位于武夷隆起北部,其含矿层位主要是侏罗系漳平组,矿体主要受北北东—北东向、北西向断裂构造控制,主矿体呈似层状产出。根据矿石结构、构造、贮存状态以及围岩蚀变等特征,认为该矿床属次火山热液充填型。
The Huangbaikeng led and zinc （copper and Silver） deposit is situated at the northern part of the Wuyi uplift. The ore-bearing beds are mostly discovered in the strata of Jurassic Zhangping Formation and the ore body is controlled by the faulted structures with the north- northeast and east-northeast trend and the northwest trend. The main orebody exists as a quasi-layer. Based on the characteristics of the ore textures and structures, the storage conditions and the wall-rock alteration, it is considered that the mineral deposit belongs to the deposit of the subvolcanic hydrothermal filling type.
出处
《福建地质》
2008年第4期361-368,共8页
Geology of Fujian
关键词
铅锌(铜银)矿床
地质特征
找矿标志
上饶黄柏坑
led and zinc deposit, geologic characteristics, ore-hunting indicator, Shangrao area, Jiangxi Province
