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Low-iron polymorphs in the pyrrhotite group
Published/Copyright:
July 28, 2010
Abstract
Two naturally-occurring low-iron pyrrhotite superstructures, based on the NiAs structure, have been confirmed. High-temperature precession photographs show that the transformation from the 4C structure to the NiAs structure occurs at 225 ± 10°C and is unrelated to the magnetic transition above 300°C. A new superstructure, also based on the NiAs structure, has been produced by quenching.
Published Online: 2010-07-28
Published in Print: 1968-01
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