对晴隆老万厂金矿、喀斯特红土、相关岩石(矿石)进行了常量元素地球化学比较研究;阐明了矿床的地球化学特征。分析指出,本类红土型金矿的矿源物质是高硅质(石英SiO2)、富铁质(黄铁矿等)的富金矿(岩)石。在崩塌、垮塌后堆积于喀斯特负地形的容矿系统的漫长风化成矿过程中,除原始矿体的风化外,同时伴随和掺合着喀斯特红土的成土作用。此种作用使矿石具有红土型的特征,并对原始金矿的风化产物的金品位有贫化作用。 A comparative study on the elemental geochemistry of the Qinglonglaowanchang gold deposit, karst laterite and related rocks (ore) has been carried out. The geochemical characteristics of the deposit have been elucidated. Analysis pointed out that this type of lateritic gold mine minerals are high silica (quartz SiO2), iron rich (pyrite, etc.) rich gold rock (rock). During the long weathering and ore-forming process of the ore-hosting system that accumulated in the karst negative terrain after the collapse and collapse, besides the weathering of the original ore body, the karst lateritic soil was accompanied and admixed at the same time. This effect has the characteristics of lateritic-type ores and depletion of the gold grade of the weathering products of the original gold mine.