ArticleProceedings of the National Academy of Sciences of the United States of America2020
High-pressure elastic properties of dolomite melt supporting carbonate-induced melting in deep upper mantle.
Article in Proceedings of the National Academy of Sciences of the United States of America, 2020. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 3 papers.
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3 citing papers in PubMed, 31 citations in OpenAlex.
- Upper mantle low-velocity layer tied to volatile-charged carbonate melts.Science advances · 2026Article
- Carbonate-Metal Reactions in the Lower Mantle.ACS earth & space chemistry · 2024Article
- The Speciation and Coordination of a Deep Earth Carbonate-Silicate-Metal Melt.Journal of geophysical research. Solid earth · 2022Article
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7 authors at 4 institutions in 2 countries.
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Abstract
Deeply subducted carbonates likely cause low-degree melting of the upper mantle and thus play an important role in the deep carbon cycle. However, direct seismic detection of carbonate-induced partial melts in the Earth's interior is hindered by our poor knowledge on the elastic properties of carbonate melts. Here we report the first experimentally determined sound velocity and density data on dolomite melt up to 5.9 GPa and 2046 K by in-situ ultrasonic and sink-float techniques, respectively, as well as first-principles molecular dynamics simulations of dolomite melt up to 16 GPa and 3000 K. Using our new elasticity data, the calculated V
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