Does infiltration of core material into the lower mantle affect the observed geomagnetic field?
- 30 September 1992
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 73 (1-2) , 29-37
- https://doi.org/10.1016/0031-9201(92)90105-5
Abstract
No abstract availableKeywords
This publication has 27 references indexed in Scilit:
- High‐pressure and high‐temperature reactions between silicates and liquid iron alloys, in the diamond anvil cell, studied by analytical electron microscopyJournal of Geophysical Research, 1992
- Exchange of angular momentum between the core and the mantle.Journal of geomagnetism and geoelectricity, 1991
- THE NATURE OF THE EARTH'S COREAnnual Review of Earth and Planetary Sciences, 1990
- 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
- High-pressure electrical resistivity measurements of Fe2O3: Comparison of static-compression and shock-wave experiments to 61 GPaSolid State Communications, 1986
- Present seismic evidence for a boundary layer at the base of the mantleJournal of Geophysical Research, 1983
- Melting of iron under core conditionsGeophysical Research Letters, 1980
- The late 1960's secular variation impulse: Further constraints on deep mantle conductivityPhysics of the Earth and Planetary Interiors, 1980
- The effect of pressure on the electrical resistivity of water-saturated crystalline rocksJournal of Geophysical Research, 1965