The excess temperature of plumes rising from the core-mantle boundary
Author:
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://www.agu.org/journals/gl/v023/i024/96GL03311/96GL03311.pdf
Reference18 articles.
1. Temperatures in the Earth's core from melting-point measurements of iron at high static pressures;Boehler;Nature,1993
2. Thermal expansion measurements at very high pressure, systematics, and a case for a chemically homogeneous mantle;Chopelas;Geophys. Res. Lett.,1989
3. Instability of a hot boundary layer and initiation of thermo-chemical plumes;Christensen;Ann. Geophys.,1984
4. Fluid dynamic and geochemical aspects of entrainment in mantle plumes;Hauri;J. Geophys. Res.,1994
5. Convection in a compressible fluid with infinite Prandtl number;Jarvis;J. Fluid Mech.,1980
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