摘要
湘南红土型金矿的分布受东西向基底断裂和深源同熔型岩浆岩控制，矿体富集受浅部断裂、岩体接触带、一定的地层层位等因素控制。本文描述了已知红土型金矿的地质特征，分析了其控矿因素。
Distribution of Laterite Au deposits in Southern Hunan is controlled by NW orientation basement faults and anaectic syntecticmagmatite, orebody enrichment is controlled by suprafault,lithosome contact zone and the fixed stratum horizon.The geological characteristics of some laterite Au deposits are discribed,in this artical,their factors-controlled are analyzed.
出处
《湖南地质》
1999年第2期79-83,共5页
Hunan Geology
关键词
红土型金矿
地质特征
控矿因素
湘南
金矿床
Laterite Au deposit,Geological characteristics,Factor-controlled,Southern Hunan.
