Abstract
Pyrrhotite, Fe1-xS, consists of a number of discrete, but structurally similar compounds (e.g. Morimoto et al., 1970; Amelinckx and Van Landuyt, Chapter 2.3 of this volume; Nakazawa et al., Chapter 5.2 of this volume) related through superstructuring of a hexagonal (a = 3.45Å ≡ A, ~5.8 Å ≡ C) subcell. Non-integral as well as integral superstructures apparently result from vacancy ordering (Ovanesyan et al., 1971). High resolution electron microscopy is a logical tool for studying vacancy distributions in pyrrhotite, and has been used to explain c-superstructure spacings (Nakazawa et al., 1974; Pierce and Buseck, 1974).
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Pierce, L., Buseck, P.R. (1976). A Comparison of Bright Field and Dark Field Imaging of Pyrrhotite Structures. In: Wenk, HR. (eds) Electron Microscopy in Mineralogy. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-66196-9_7
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DOI: https://doi.org/10.1007/978-3-642-66196-9_7
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