Figure 1
From: Complete agreement of the post-spinel transition with the 660-km seismic discontinuity

Phase boundaries of the post-spinel transition in Mg2SiO4. Data points were calculated based on the Tange 3BM MgO scale11. Open and solid circles with error bars identify the stable phases as ringwoodite and bridgmanite + periclase, respectively. The black solid line is the expected condition of the 660-km discontinuity7,8,16,17,18,19,20,21. The red (T-3BM) and blue (T-Vinet) solid lines are phase boundaries evaluated using the fixed points obtained in this study and the Clapeyron slopes of ref.4 after re-calculation with the Tange 3BM and Vinet MgO scales, respectively. The purple dashed line [F04 (S-3BM)] is the original phase boundary determined by ref.4 using the MgO scale proposed by ref.12. The aforementioned red [F04 (T-3BM)] and blue [F04 (T-Vinet)] dashed lines are therefore the phase boundaries recalculated from the original data of ref.4 using the specified scales. Brg: bridgmanite; Pc: periclase; Rw: ringwoodite.