期刊
ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES, VOL 41
卷 41, 期 -, 页码 657-+出版社
ANNUAL REVIEWS
DOI: 10.1146/annurev-earth-050212-124007
关键词
ultrahigh pressure; phase relation; composition; thermal evolution; stratification
资金
- Directorate For Geosciences [1160917] Funding Source: National Science Foundation
- Grants-in-Aid for Scientific Research [24000005] Funding Source: KAKEN
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.
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