U-Nb's discontinuous precipitation, γ bcc matrix → α orth cellular + γ bcc cellular , is intriguing in the sense that it allows formation and growth of the metastable γ phase during the course of its occurrence. Previous attempts to explain the thermodynamic origin of U-Nb's discontinuous precipitation hypothesized that the energy of α forms an intermediate common tangent with the first potential of the double-well energy of γ at the γ composition. While this hypothesis is eligible and consistent with the experimental observation of gradual increase in γ composition at increasing temperature, it is in conflict with recent experiments whose results indicated a distribution of γ compositions in the vicinity of 50 at%Nb. To shed some light onto this issue, the current work investigates the origin of U-Nb's discontinuous precipitation in view of fundamental thermodynamics and kinetics, taken from the perspective of phase-field theory. It has been showed that local misfit strain tends to play a crucial role in the formation and growth the discontinuous precipitation. Depending on the magnitude of strain developed at grain boundaries, either an increasing γ composition or a random distribution of γ composition around the equiatomic value with respect to increasing temperature could be expected.