Compared with Lehua manganese deposit in Pingxiang-Leping faulted basin, which is a sedimentary hydrothermal superimpose并与萍一乐断陷盆地内的沉积加热液叠改型乐华锰矿床进行了对比分析，二者在矿体规模、矿石类型、锰品位等方面存在显著差别，应属不同成因类型的矿床。