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。
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.
出处
《江苏地质》
1998年第1期27-30,共4页
Jiangsu Geology
