The 6722 vein-type Uranium Deposit, the largest deposit in Hecaokeng uranium ore fields, lies in the intersection of EW-trending Nanling Mountains and NE-trending Wuyi uplift.In this study, eight samples of syngenic calcite from granite-type ore body were collected for Sm-Nd isochron age dating, and the result was (113.4±6.9) Ma. Early-stage mineralization happening in 113 Ma preceded main-stage mineralization in felsic cryptoexplosive breccia. It is inferred that early-stage mineralization (113 Ma) created preconcentration of uranium for the formation of later higher-grade ore in cryptoexplosive breccia.