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江苏某地红土型金矿地质特征及成矿机理分析
引用本文:邱祖林,陈福鑫.江苏某地红土型金矿地质特征及成矿机理分析[J].地质学刊,1998,22(1):27-30.
作者姓名:邱祖林  陈福鑫
作者单位:江苏省地质矿产勘查开发公司
摘    要:江苏某处金矿为渗流热卤水—次生富集沉积成因,工业类型属改造红土型金矿床,矿石类型主要为含泥化角砾红土金矿石,成矿物质最终源于含金碳盐岩地层,受构造、地下(热)水及气候等因素控制。

关 键 词:红土型金矿  成矿作用  第四系  江苏

Geological features and Analysis of Ore-Forming Mechanism for Lateritic Gold Deposit in Somewhere in Jiangsu Province
Qiu Zulin Chen Fuxin Corporation of Exploration and Development of Geologic and Minerals,Jiangsu Province,Nanjing.Geological features and Analysis of Ore-Forming Mechanism for Lateritic Gold Deposit in Somewhere in Jiangsu Province[J].Jiangsu Geology,1998,22(1):27-30.
Authors:Qiu Zulin Chen Fuxin Corporation of Exploration and Development of Geologic and Minerals  Jiangsu Province  Nanjing
Institution:Qiu Zulin Chen Fuxin Corporation of Exploration and Development of Geologic and Minerals,Jiangsu Province,Nanjing,210018
Abstract:Located in the eastern suburbs of Nanjing, Jiangsu Province,the gold deposit is a small scale opencut mine. It belongs to a sedimentarygenesis of seepage hot brine-secondary enrichment. Industrial type of the deposit belongs to a remoulded lateritic gold deposit. The lateritic gold ore with argillized breccia is main ore type. Metallogenetic matter originated from finally gold bearing carbonate rock strata under the control of strctures, underground thermal water and climate etc. according to the geological works and drilling hole data.
Keywords:Lateritic  gold  deposit  Ore  forming  process  Quaternary  Jiangsu
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