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竹子坑铅锌矿地质特征与成因分析

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竹子坑铅锌矿处在"粤北山字型构造"的前弧东翼,翁城复向斜内.出露地层主要有上古生界泥盆系(D)、石炭系(C),中生界侏罗系(J)及新生界第四系(Q)等,矿床成因类型属中低温热液充填交代型矿床.通过分析区域地质背景、矿区、矿体地质特征及矿石质量等,总结出矿区铅锌矿床地质特征与成因,为以后地质找矿提供重要的参考指示意义.
Geological Characteristics and Genesis Analysis of Zhuzikeng Lead-zinc Mine
The Zhuzikeng lead-zinc mine is located on the eastern wing of the front arc of the"山-type tectonic system in northern Guangdong",within the Wengcheng syncline.The exposed strata mainly include the Upper Paleozoic Devonian(D),Carboniferous(C),Mesozoic Jurassic(J),and Cenozoic Quaternary(Q).The genesis type of the deposit belongs to the medium low temperature hydrothermal filling and metasomatism type.This article summarizes the geological characteristics and genesis analysis of lead-zinc deposits in the mining area by analyzing the regional geological background,mining area,ore body geological features,and ore quality,providing important reference and guidance for future geological exploration.

Zhuzikeng lead zinc minegeological featurescause analysis

龙勇

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广东省有色金属地质局九四○队,广东 清远 511500

竹子坑铅锌矿 地质特征 成因分析

2024

山西冶金
山西省金属学会 山西省有色金属学会

山西冶金

影响因子:0.139
ISSN:1672-1152
年,卷(期):2024.47(11)