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河台金矿蚀变糜棱岩型金矿床成因探讨
引用本文:龚朝阳.河台金矿蚀变糜棱岩型金矿床成因探讨[J].黄金科学技术,2004,12(4):4-6.
作者姓名:龚朝阳
作者单位:广东高要河台金矿,广东,高要,526127
摘    要:自20 世纪80 年代初由民采发现河台金矿韧性剪切带含金蚀变糜棱岩型矿床以来,国家投入大量人力物力找矿,也引起广大地质工作者极大关注。通过对其与赋存条件有关的地层、构造及岩浆岩的分析研究,发现河台金矿韧性剪切带含金蚀变糜棱岩型矿床的成因与液态矿源从形成、运移及经过后期构造运动的改造具有密切关系。

关 键 词:蚀变糜棱岩  成因  液态矿源  二次迁移
文章编号:1005-2518(2004)04-0004-03
收稿时间:2004-03-10
修稿时间:2004年3月10日

Mineralization Study on Metamorphosed Mylonite Gold Deposit of Hetai Gold Mine
GONG,Zhao-yang.Mineralization Study on Metamorphosed Mylonite Gold Deposit of Hetai Gold Mine[J].Gold Science and Technololgy,2004,12(4):4-6.
Authors:GONG  Zhao-yang
Affiliation:Hetai Gold Mine,Guangdong Gaoyao 526127,China
Abstract:Since Hetai Gold Mine as auriferous ductile shear zone metamorphosed mylonite gold deposit was found in 1980's by civil mining, the government invested a lot in exploration of gold deposits, and it also caught many geological workers' attention. Through study on stratum, tectonics and magma rock relevant to its existence, conclusion is made that mineralization of auriferous ductile shear zone metamorphosed mylonite gold deposit of Hetai Gold Mine has a close relation to formation, transfer and geotectonic evolution of fluidity mineral resources.
Keywords:metamorphosed mylonite  mineralization  fluidity mineral resources  secondary transfer  
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