Extended Data Figure 7: The CPO of forsterite grains in a Fo+Di sample (KF-172).
From: Olivine crystals align during diffusion creep of Earth’s upper mantle
The sample was statically annealed at 1,330 °C for 10 h and then deformed under compression (ε = 0.6) at 1,200 °C. The initial grain size of this sample before the creep test was already large (Extended Data Table 1).
