Natural and synthetic ferroselite : A roentgenographic mimesis of rammelsbergite

Details Natural and synthetic ferroselite : A roentgenographic mimesis of rammelsbergite Natural and synthetic ferroselite : A roentgenographic mimesis of rammelsbergite

Nov 1958

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1958gecoa..15...73k&link_type=abstract

Geochimica et Cosmochimica Acta, vol. 15, Issue 1-2, pp.73-79

Physics

1

Scientific paper

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 and (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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