Abstract
Smythite and monoclinic Fe3S4 have been identified by X-ray diffraction procedures in quenched ironsulfide compositions. Both phases appear to be metastable under the conditions of the experiments and their development is structurally induced.
Smythite occurs as a coherent twinned intergrowth with hexagonal 3C pyrrhotite. Individual single crystals contain about 50% smythite. Reciprocal lattice rows with h-k ≠ 3n show continuous diffraction streaks. The available data suggest that smythite forms via a “polytypic” displacive transformation, by the introduction of stacking faults in the hexagonal close-packed layers of S atoms in high-temperature 1C pyrrhotite. This is analogous to the transformation of 2H wurtzite to intermediate ordered and disordered ZnS layer sequences. The ideal formula of smythite appears to be Fe13S16.
Monoclinic Fe3S4 (a=5.93, b=3.42, c=10.64 Å, β=91.9°) is present in amounts up to 25% of total sulfides. It has a derivative NiAs-type structure, and is isomorphous with monoclinic Cr3S4 and Fe3Se4. It occurs as small lenticular lamellae within grains of 3C pyrrhotite, and apparently corresponds to the unidentified lamellar phase of Arnold (1962). The lamellae have a rhombohedral morphology, with a habit plane close to {1011}. In single crystal grains of pyrrhotite, monoclinic Fe3S4 in twinned in a manner consistent with transformation from high-temperature 1C pyrrhotite. Although Fe3S4 lamellae have the general appearance of plate martensite, they do not represent a diffusionless transformation.
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Fleet, M.E. Synthetic smythite and monoclinic Fe3S4 . Phys Chem Minerals 8, 241–246 (1982). https://doi.org/10.1007/BF00308244
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DOI: https://doi.org/10.1007/BF00308244