Fig. 9From: Formation mechanisms of ringwoodite: clues from the Martian meteorite Northwest Africa 8705Pressure–temperature phase diagram for olivine (Fo65) after Ito and Takahashi (1989), Frost (2008), Tomioka and Miyahara (2017). The shaded region corresponds to the ringwoodite stability field. Bdm, bridgmanite; Mw, magnesiowüstite; others are the same as aboveBack to article page