Determination of akimotoite-bridgmanite (MgSiO3) phase transition at 1250-2050 K using a multi-anvil press with in-situ X-ray diffraction: Explanation of the 660-km discontinuity depressions beneath cold subduction zones (20 + 5 min)

1 Feb 2021, 14:00
25m
ONLINE

ONLINE

Speaker

A. Chanychev (BGI, Univ. of Bayreuth / DESY)

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