Extended Data Figure 2: The CPO of forsterite grains from tension experiments on Fo+Di samples at 1,330 °C with different amounts of strain (KS-16, ε = 1.1; KS-17, ε = 1.5).
From: Olivine crystals align during diffusion creep of Earth’s upper mantle
The CPO of the sample with the smallest strain (KS-13, ε = 0.6) is shown in Fig. 2.
