Pressure dependence of metal–silicate partitioning explains the mantle phosphorus abundance
- Location
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Deutsche Nationalbibliothek Frankfurt am Main
- Extent
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1 Online-Ressource.
- Language
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Englisch
- Bibliographic citation
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Pressure dependence of metal–silicate partitioning explains the mantle phosphorus abundance ; volume:14 ; number:1 ; day:12 ; month:1 ; year:2024 ; pages:1-8 ; date:12.2024
Scientific reports ; 14, Heft 1 (12.1.2024), 1-8, 12.2024
- Creator
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Ikuta, Nagi
Sakamoto, Naoya
Tagawa, Shoh
Hirose, Kei
Tsutsumi, Yutaro
Yokoo, Shunpei
Yurimoto, Hisayoshi
- Contributor
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SpringerLink (Online service)
- DOI
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10.1038/s41598-024-51662-y
- URN
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urn:nbn:de:101:1-2024032515162679040748
- Rights
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Last update
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14.08.2025, 10:53 AM CEST
Data provider
This object is provided by:
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Deutsche Nationalbibliothek. If you have any questions about the object, please contact the data provider.
Associated
- Ikuta, Nagi
- Sakamoto, Naoya
- Tagawa, Shoh
- Hirose, Kei
- Tsutsumi, Yutaro
- Yokoo, Shunpei
- Yurimoto, Hisayoshi
- SpringerLink (Online service)
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Oxidation state of Cu in silicate melts at upper mantle conditions
Thermodynamic controls on element partitioning between titanomagnetite and andesitic–dacitic silicate melts
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The solubility of N2 in silicate melts and nitrogen partitioning between upper mantle minerals and basalt
Dynamics of self-reorganization explains passivation of silicate glasses
Carbon-bearing silicate melt at deep mantle conditions
Trace element partitioning between pyrochlore, microlite, fersmite and silicate melts
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