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Navrotsky 1980
Navrotsky, A. (1980). Lower mantle phase transitions may generally have negative pressure-temperature slopes. Geophysical Research Letters 7: doi: 10.1029/GL007i009p00709. issn: 0094-8276.

Phase transitions in oxides at pressures above about 150 kbar may commonly have negative pressure-temperature slopes. The causes of the higher entropies of denser phases include low frequency vibrations of small atoms in sites having high coordination number and long metal-oxygen distances, decrease in directional bonding, postional disorder and possible solid-electrolyte behavior, and semiconductor-metal and metal-metal transitions.

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Geophysical Research Letters
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