Abstract
Iron diselenide (FeSe 2) has been synthesized in sealed, evacuated, silica-glass tubes at temperatures between 450 and 550°C. Its powder pattern is identical with that of ferroselite described by Buryanova and Komkov (1955). The first fifteen lines of the pattern are indistinguishable from those of rammelsbergite (NiAs 2). Single crystals of ferroselite from Temple Mountain, Utah, were studied on the precession camera. Their diffraction patterns are also deceivingly similar to those of rammelsbergite.
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