Meteorites and thermodynamic equilibrium in f.c.c. iron-nickel alloys (25 - 50%Ni).

Mossbauer spectroscopy and X-ray investigations show that taenite (f.c.c. iron-nickel alloy) in meteorites generally has decomposed into an ordered phase FeNi with the L10 structure and a disordered f.c.c. iron-nickel alloy containing less than 25% of Ni. The two phases have the same bravais lattice, i.e., they form a pseudo monocrystal. The decomposition is discussed in terms of Fe-Ni phase diagram.

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