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The p1̅ to I1̅ phase transition in end-member anorthite, CaAl 2 Si 2 O 8 , has been reversed in-situ at high pressures and temperatures in an internally heated diamond-anvil pressure cell using single-crystal X-ray diffraction. The unit-cell parameters of anorthite were determined at 48 temperature-pressure points up to 255 °C and 2.6 GPa.

Reversed brackets for the P1̅= I1̅ transition in anorthite at high pressures and temperatures