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黔东地区铅锌矿地质特征及成矿作用分析
引用本文:陈国勇,安琦,范玉梅.黔东地区铅锌矿地质特征及成矿作用分析[J].贵州地质,2005,22(4):252-259.
作者姓名:陈国勇  安琦  范玉梅
作者单位:贵州省地质调查院,贵州,贵阳,550004
摘    要:本文根据控矿构造格局,将黔东地区铅锌矿划为扬子准地台东缘、华南褶皱带西缘,以及扬子准地台与华南褶皱带过渡带等三个铅锌矿带,并分别对其典型矿床进行了解剖和特征描述。在此基础上,分析了铅锌矿成矿作用,将黔东地区铅锌矿分为准同生沉积型铅锌矿床和热液交代一充填型铅锌矿床两种成因类型,综述了相应的控矿条件及矿床成因。最后,进行了黔东地区铅锌矿找矿远景分析,提出了6个找矿远景区。

关 键 词:铅锌矿  地质特征  成矿作用  黔东地区  贵州
文章编号:1000-5943(2005)04-0252-08
收稿时间:2005-12-10
修稿时间:2005年12月10

Geologic Characteristic of the Lead-Zinc Deposits in the Eastern Guizhou and Analysis on Metallogenesis
CHEN Guo-yong,AN Qi,FAN Yu-mei.Geologic Characteristic of the Lead-Zinc Deposits in the Eastern Guizhou and Analysis on Metallogenesis[J].Guizhou Geology,2005,22(4):252-259.
Authors:CHEN Guo-yong  AN Qi  FAN Yu-mei
Abstract:In this paper, the lead-zinc deposits in the eastern Guizhou are divided into three lead-zinc belts including east rim of Yangtgz para-platform, west rim of the South China folds belt and their transition zone according to the structural framework of controlling, which typical deposits are anatomized and the characteristic are depicted. Furthermore, the feature of lead-zinc metallogenesis is generalized, two types of origin are of the para -synchronic sedimentary lead-zinc deposits and hydrothermal replacement-infill type of lead-zinc deposits, corresponding controlling conditions and deposit origin are synthetically stated. Finally, studies of prospecting for the lead-zinc deposit in the eastern Guizhou is carried out with six prospeering zones presented.
Keywords:lead-zinc deposits  geologic attributes  minerogenesis  eastern area of Guizhou
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