Thermal and magnetic constraints on the cooling of the Earth.

Details Thermal and magnetic constraints on the cooling of the Earth. Thermal and magnetic constraints on the cooling of the Earth.

Mar 1984

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1984geoji..76..653m&link_type=abstract

Geophysical Journal International, Vol. 76, No. 3, p. 653 - 666

Physics

Earth:Cooling

Scientific paper

The thermodynamic requirements of a dynamo in the Earth's core can be
expressed in terms of the heat flux from core to mantle. That heat flux
is estimated from a simple layered model of the Earth, using
parameterized convection theory to calculate the heat transport through
the mantle.

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