The intermixing of Fe and T ͑TϭCr,W͒ during ball milling of elemental powder mixtures Fe 1Ϫx T x , with xϭ0.70 for TϭCr and xϭ0.50 for TϭW, has been followed by 57 Fe Mössbauer spectroscopy at room temperature ͑RT͒ and by magnetization measurements for TϭW. The chemical compositions have been chosen to yield final alloys or compounds which are nonmagnetic at RT to better follow the evolution of magnetic phases with milling times. For a long period of milling time t m before reaching the final stationary state, the hyperfine magnetic field distributions remain stationary in shape for both TϭCr and TϭW. Only the relative weight of the magnetic contribution decreases with t m . For TϭW, the average moment of magnetic Fe atoms is further shown to remain constant with t m . Stationary hyperfine field distribution shapes are found to be similar not only for TϭCr and W but also for TϭSi ͑xϭ0.50͒ while published spectra suggest to add TϭAl, Ti, V, Ta, Re to the latter nonexhaustive list. The stationary shape is characterized by a narrow peak located at a field close to the field of alpha iron at RT ͑330 kG͒ and by a broad, almost featureless, band from ϳ50-100 kG to ϳ300-320 kG. The broad band represents about 2/3 of the normalized field distribution. We deduce that the interpretation which consists in attributing the x-ray diffraction peaks of Fe-based bcc solid solutions to a single Fe-rich homogeneous solid solution must be done with care for intermediate milling times. We cannot infer from such hyperfine measurements a detailed description of the regions of the powders which are responsible for such magnetic features. We argue however that irregular interfaces between nanometer-sized Fe-rich zones and T-rich zones may play a role to explain the observed shape of the hyperfine field distributions. The general conditions ͑process and materials͒ in which such phenomena may occur remain to be clarified. ͓S0163-1829͑96͒07941-6͔