Composition and State of the Core
The composition and state of Earth's core, located deeper than 2,900 km from the surface, remain largely uncertain. Recent static experiments on iron and alloys performed up to inner core pressure and temperature conditions have revealed phase relations and properties of core materials. These m...
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| Veröffentlicht in: | Annual review of earth and planetary sciences 2013-01, Vol.41 (1), p.657-691 |
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| container_end_page | 691 |
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| container_issue | 1 |
| container_start_page | 657 |
| container_title | Annual review of earth and planetary sciences |
| container_volume | 41 |
| creator | Hirose, Kei Labrosse, Stéphane Hernlund, John |
| description | The composition and state of Earth's core, located deeper than 2,900 km from the surface, remain largely uncertain. Recent static experiments on iron and alloys performed up to inner core pressure and temperature conditions have revealed phase relations and properties of core materials. These mineral physics constraints, combined with theoretical calculations, continue to improve our understanding of the core, in particular the crystal structure of the inner core and the chemical composition, thermal structure and evolution, and possible stratification of the outer core. |
| doi_str_mv | 10.1146/annurev-earth-050212-124007 |
| format | Article |
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Recent static experiments on iron and alloys performed up to inner core pressure and temperature conditions have revealed phase relations and properties of core materials. 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| fulltext | fulltext |
| identifier | ISSN: 0084-6597 |
| ispartof | Annual review of earth and planetary sciences, 2013-01, Vol.41 (1), p.657-691 |
| issn | 0084-6597 1545-4495 |
| language | eng |
| recordid | cdi_proquest_miscellaneous_1786198646 |
| source | Annual Reviews Complete A-Z List |
| subjects | Alloys Crystal structure Earth Earth core Evolution Ferrous alloys Iron alloys Mathematical analysis Minerals Physics Stratification Stratigraphy Temperature effects |
| title | Composition and State of the Core |
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