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SaveSound velocity measurements of γ-(Mg0.91Fe0.09)2SiO4 show that the ringwoodite to bridgmanite and ferropericlase phase transformation does not produce the seismically observed 660 km discontinuity
Huang, Rong; Thomson, Andrew R.; Brodholt, John P.; Crichton, Wilson A.; Rosenthal, Anja; Druzhbin, Dmitrii; Backhouse, Nicholas; Taschimowitz, Isaac; Bessas, Dimitrios; Yaroslavtsev, Sergey; Wang, Biao
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