Fig. 1. Faults in the olivine sample deformed at 15.4 GPa and 850 ℃. (IMAGE)

Ehime University

Fig. 1. Faults in the olivine sample deformed at 15.4 GPa and 850 ℃.

Caption

Left: Recovered sample. Red dashed lines represent faults developed in the sample. Right: poirierite grains formed in a deformed olivine crystal.

Credit

Tomohiro Ohuchi

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