<p>The study reports textures and compositions of uraninite and brannerite from the Mohuldih uranium deposit of the Singhbhum Shear Zone. Three types of texturally varied uraninite are identified: (i) pre-tectonic (U_G−1), (ii) syn to post-tectonic (U_G−2), and (iii) inclusions (U_G−3). Based on UO₂ and PbO composition, these are further divided into five subgroups (U_G−1a, U_G−2a, U_G−1b, U_G−2b, and U_G−3). The negative correlation between the rare-earth elements including Y (ΣREE₂O₃ + Y₂O₃) and UO₂ of U_G−1a and U_G−2a uraninite indicates substitution of REE and Y for U⁴⁺ in the structure of these grains during primary crystallization, whereas U_G−1b and U_G−2b resulted from REE + Y + U-enrichment during secondary fluid-induced alteration. Compositional trends further reveal post-crystallization incorporation of Na, Si, K, Ca, Ti, and Fe, replacing radiogenic Pb in the structure of uraninite. The U-Th-Pb_Total dating of uraninite yields two clusters: older (~ 1.71−1.64 Ga; preserved by U_G−1a and U_G−2a) and younger (~ 0.93 Ga; U_G−1b and U_G−2b). Additionally, the extrapolated best-fit linear trend for uraninite in U_G−3 population preserves chemical dates ranging from ~ 1.71 to ~ 1.64 Ga. The ~ 1.64 Ga represents a U + Y + HREE + Ca + Fe hydrothermal event, resulting in the precipitation of uraninite, followed by dissolution-reprecipitation of the mineral along the grain boundary and fractures at ~ 0.93 Ga. The oldest mesured date (~ 1.71 Ga) is attributed to partial Pb-loss by older uraninite during the ~ 1.64 Ga hydrothermal event, with no evident geological significance in the area. The dissolution-reprecipitation of the early-formed uraninite also resulted in the formation of brannerite and ilmenite during the ~ 0.93 Ga event.&#xa0;</p>