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贵州西部玄武岩分布区大麦地金矿成矿地质特征
引用本文:吴小红,程鹏林,肖成刚,马健. 贵州西部玄武岩分布区大麦地金矿成矿地质特征[J]. 贵州地质, 2013, 0(4): 283-288
作者姓名:吴小红  程鹏林  肖成刚  马健
作者单位:[1]贵州省地矿局105地质大队,贵州贵阳550018 [2]贵州省地矿局115地质大队,贵州清镇551400
基金项目:本文得到中国地质调查局“贵州贞丰整装勘查区金-铀多金属控矿因素研究”项目(12120113094400)资助.
摘    要:大麦地金矿为赋存于峨眉山玄武岩组与茅口组之间因区域构造和热液蚀变作用形成的构造蚀变体(Sbt)中的原生中型金矿床,位于贵州西部峨眉山玄武岩分布区盘县莲花山背斜南东翼.本文系统总结大麦地金矿详查成果,以期对莲花山背斜区域原生金矿找矿提供参考,初步认为贵州西部玄武岩分布区原生金矿找矿具有较大的潜力.

关 键 词:大麦地  玄武岩  金矿  原生矿  盘县  贵州

Metallogenic Geologic Characteristics of Damaidi Gold Deposit in Basalt Distribution Area of Western Guizhou
WU Xiao-hong,CHENG Peng-lin,XIAO Cheng-gang,MA Jian. Metallogenic Geologic Characteristics of Damaidi Gold Deposit in Basalt Distribution Area of Western Guizhou[J]. Guizhou Geology, 2013, 0(4): 283-288
Authors:WU Xiao-hong  CHENG Peng-lin  XIAO Cheng-gang  MA Jian
Affiliation:1. Geologic Party 105, Guizhou Bureau of Geology & Mineral Exploration and Development, Guiyang 550018, Guizhou, China; 2. Geologic Party 115, Guizhou Bureau of Geology & Mineral Exploration and Development, Qingzhen 551400, Guizhou, China)
Abstract:Damaidi gold deposit is primary middle gold deposit which occurs in the structural alteration body formed by regional structure and geothermal alteration between Xuanwuyan formation and Maokou forma- tion of E' meishan, it situated in southeast anticline of Lianhuashan in Panxian where the basalt distributed. In this paper, the Damaidi gold deposit survey is summarized for primary gold exploration in anticline area of Li- anhuashan, it' s thought the primary gold deposit ezploration in basalt distribution area of western Guizhou.
Keywords:Damaidi  Basalt  Gold deposit  Primary Deposit  Panxian  Guizhou
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