“…The transition into equilibrium state goes by phase decomposition into g-and a-phases in the case of lowtemperature annealing [7,18,19], or paramagnetic g par and ferromagnetic NiFe phases, as it was found in meteorites [4][5][6], electronic beam irradiated samples [7,20,21] and samples prepared using mechanical alloying [22][23][24][25][26][27]. The paramagnetic g par and ferromagnetic NiFe phases are indistinguishable by diffraction methods; therefore, their cell parameters are accepted to be the same.…”