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6722铀矿床位于赣南会昌地区,在大地构造上位于EW向南岭构造带与NE向武夷隆起带交汇部位。矿区出露印支期富城多期复式花岗岩体,锆石LA-ICP-MS法测得其主体年龄年210～240Ma(周新民,2007)。6722矿床中矿体主要呈不规则凸镜状、似层状及团块状产出在受草桃背火山机构控制的隐爆角砾
The 6722 uranium deposit is located in the Huichang area of southern Jiangxi Province and is located on the earth structure at the junction of the EW-Nanling structural belt and NE-Wuyi uplift belt. The Indosinian multi-stage multi-granite body from Indosinian is exposed in the mines. The main body age is 210-240 Ma measured by zircon LA-ICP-MS (Zhou Xinmin, 2007). The ore bodies in the 6722 ore deposit are mainly irregularly convex and mirror-like in shape, like stratified and massive output in the cryptotoxi breccia controlled by the grass peach back volcano body