A Hybrid Mechanism for Enhanced Core‐Mantle Boundary Chemical Interaction
Author:
Affiliation:
1. Earth‐Life Science Institute, Tokyo Institute of Technology Meguro 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/10.1029/2021GL094456
Reference45 articles.
1. An early geodynamo driven by exsolution of mantle components from Earth’s core
2. Metal–silicate partitioning of Pb and U: Effects of metal composition and oxygen fugacity
3. The debate over core–mantle interaction
4. 186Os and 187Os enrichments and high-3He/4He sources in the Earth’s mantle: Evidence from Icelandic picrites
5. Sediments at the Top of Earth's Core
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3. The Origin of Earth's Mantle Nitrogen: Primordial or Early Biogeochemical Cycling?;Geochemistry, Geophysics, Geosystems;2022-05
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