The Earth's 'missing' niobium may be in the core.
As the Earth's metallic core segregated from the silicate mantle, some of the moderately siderophile ('iron-loving') elements such as vanadium and chromium are thought to have entered the metal phase, thus causing the observed depletions of these elements in the silicate part of the E...
Prif Awduron: | Wade, J, Wood, B |
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Fformat: | Journal article |
Iaith: | English |
Cyhoeddwyd: |
2001
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Eitemau Tebyg
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Core formation and the oxidation state of the Earth
gan: Wade, J, et al.
Cyhoeddwyd: (2005) -
Accretion of the Earth and segregation of its core.
gan: Wood, B, et al.
Cyhoeddwyd: (2006) -
Niobium and Niobium Compounds
gan: Eckert, J.
Cyhoeddwyd: (1993-01-01) -
Enriched lithospheric mantle storage of the Earth's missing niobium: New insights from alkaline rocks with superchondritic Nb/Ta ratios
gan: Yan Yang, et al.
Cyhoeddwyd: (2024-08-01) -
Potassium in the Earth's core?
gan: Gessmann, C, et al.
Cyhoeddwyd: (2002)