High‐pressure metallization of FeO and implications for the Earth's core
- 7 December 1986
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 13 (13), 1541-1544
- https://doi.org/10.1029/gl013i013p01541
Abstract
No abstract availableThis publication has 15 references indexed in Scilit:
- Metallization of Fe0.94O at elevated pressures and temperatures observed by shock-wave electrical resistivity measurementsSolid State Communications, 1986
- Static compression of wüstite (Fe0.98O) to 120 GPaJournal of Geophysical Research, 1985
- A lower mantle S-wave triplication and the shear velocity structure of D''Geophysical Journal International, 1983
- Thermodynamics of the system Fe--FeO--MgO at high pressure and temperature and a model for formation of the Earth's coreGeophysical Journal International, 1983
- The Equation of State for Iron and the Earth’s CorePublished by Springer Science and Business Media LLC ,1982
- Models of the Earth's CoreScience, 1981
- Cesium chloride versus nickel arsenide as possible structures for (Mg, Fe)O in the lower mantleJournal of Geophysical Research, 1981
- Equations of state of FeO and CaOGeophysical Journal International, 1980
- Electrical and optical properties of FeOJournal of Solid State Chemistry, 1975
- Electrical conductivity, demagnetization, and the high-pressure phase transition in shock-compressed ironSolid State Communications, 1969