Figure 5 | Scientific Reports

Figure 5

From: Cubic Fe-bearing majorite synthesized at 18–25 GPa and 1000 °C: implications for element transport, subducted slab rheology and diamond formation

Figure 5The alternative text for this image may have been generated using AI.

(a) Nano-Infrared spectra collected on two areas of samples M81 corresponding to the polycrystalline matrix (red continuous line) and the Re-ReO2 buffer (blue dotted line) for comparison. (b) Nano-Infrared spectrum collected on M81 polycrystalline matrix.

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