Some thermal consequences of a gravitationally powered dynamo

Author:

Loper David E.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference34 articles.

1. Structure of the F layer and reasons for convection in the earth's core;Braginsky;Dokl. Akad. Nauk SSSR,1963

2. The magnetic field within the earth;Bullard;Proc. Roy. Soc. London, Ser. A,1949

3. Comment on paper by G. Higgins and G. C. Kennedy, ‘The adiabatic gradient and the melting point gradient in the core of the earth, ’;Busse;J. Geophys. Res.,1972

4. Generation of magnetic fields by convection;Busse;J. Fluid Mech.,1973

5. A necessary condition for the geodynamo;Busse;J. Geophys.Res.,1975

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