Sound 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

Journal:
Earth and Planetary Science Letters
Published:
DOI:
10.1016/j.epsl.2025.119416
Affiliations:
7
Authors:
11
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Institutions Authors Share
European Synchrotron Radiation Facility (ESRF), France
4.833333
 0.44
UCL, United Kingdom (UK)
3.333333
 0.30
University of Oxford, United Kingdom (UK)
1.000000
 0.09
University of Michigan (U-M), United States of America (USA)
0.500000
 0.05
University of Oslo (UiO), Norway
0.500000
 0.05
Australian National University (ANU), Australia
0.500000
 0.05
Natural History Museum, United Kingdom (UK)
0.333333
 0.03
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