Temperatures in the Earth's core from melting-point measurements of iron at high static pressures
- 1 June 1993
- journal article
- letter
- Published by Springer Nature in Nature
- Vol. 363 (6429) , 534-536
- https://doi.org/10.1038/363534a0
Abstract
No abstract availableKeywords
This publication has 15 references indexed in Scilit:
- Melting of the FeFeO and the FeFeS systems at high pressure: Constraints on core temperaturesEarth and Planetary Science Letters, 1992
- The high‐pressure melting curve of iron: A technical discussionJournal of Geophysical Research, 1991
- Melting, thermal expansion, and phase transitions of iron at high pressuresJournal of Geophysical Research, 1990
- Theory of the iron phase diagram at Earth core conditionsJournal of Geophysical Research, 1990
- The system Fe-FeO revisitedPhysics and Chemistry of Minerals, 1990
- The Melting Curve of Iron to 250 Gigapascals: A Constraint on the Temperature at Earth's CenterScience, 1987
- The phase diagram of iron to 430 kbarGeophysical Research Letters, 1986
- Phase transitions, Grüneisen parameter, and elasticity for shocked iron between 77 GPa and 400 GPaJournal of Geophysical Research, 1986
- On the (?, ?, ?) Triple Point of Iron and the Earth's CoreGeophysical Journal International, 1975
- The Melting Relations of Iron, and Temperatures in the Earth's CoreGeophysical Journal International, 1972