Acoustic Wave Velocities of Ferrous‐Bearing MgSiO <sub>3</sub> Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle-Reference-Cited by-同舟云学术

Acoustic Wave Velocities of Ferrous‐Bearing MgSiO ₃ Glass up to 158 GPa With Implications for Dense Silicate Melts at the Base of the Earth's Mantle

Published:2022-10-10 Issue:19 Volume:49 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophysical Research Letters

Author:

Mashino Izumi¹²^ORCID,Murakami Motohiko¹^ORCID,Kitao Shinji³^ORCID,Mitsui Takaya⁴,Masuda Ryo⁵^ORCID,Seto Makoto³

Affiliation:

1. Department of Earth Sciences ETH Zürich Zürich Switzerland

2. Institute for Planetary Materials Okayama University Tottori Japan

3. Institute for Integrated Radiation and Nuclear Science Kyoto University Osaka Japan

4. Synchrotron Radiation Research Center Kansai Photon Science Institute Quantum Beam Science Research Directorate National Institutes for Quantum Science and Technology Sayo‐gun Japan

5. Graduate School of Science and Technology Hirosaki University Hirosaki‐shi Japan

Funder

Japan Society for the Promotion of Science

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2022GL098279

Reference43 articles.

1. Diamond anvil Raman gauge in multimegabar pressure range

2. Solid–liquid iron partitioning in Earth’s deep mantle

3. Structural and topological changes in silica glass at pressure

4. Melt–crystal density crossover in a deep magma ocean

5. Silicate perovskite-melt partitioning of trace elements and geochemical signature of a deep perovskitic reservoir

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