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Inversion to chalcocite (orthorhombic polymorph) at atmospheric pressure, chalcocite inversion to hexagonal polymorph at 103.5 degrees C and cubic polymorph at 420 degrees C (at atmospheric pressure)
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M. E. Fleet Phase Equilibria at High Temperatures Reviews in Mineralogy and Geochemistry, January 1, 2006; 61(1): 365 - 419. [Full Text] [PDF] |
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