Deformation mechanism maps of wadsleyite, ringwoodite and majorite garnet at transition zone conditions (IMAGE)
Caption
Deformation mechanism maps of (a) wadsleyite at 15 GPa and 1500 K, (b) ringwoodite at 20 GPa and 1700 K and (c) majorite garnet at 18 GPa and 1600 K.
Credit
Dr. S. Ritterbex (Ehime University)
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