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Thermal Analysis Curves of Oxide Minerals

The thermal properties of oxide minerals are characterized by structure transformation, melting, dehydration and valence-state changes during heating. [Pg.271]

Paratellurite—690 °C endotherm, paratellurite melts at a temperature higher than 850 °C, it evaporates. [Pg.271]

Molybdite—798 °C endotherm, molybdite melts, then it evaporates. [Pg.271]

Litharge—At a temperature higher than 300 °C, litharge transforms to massicot. [Pg.271]

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