Physics
Scientific paper
May 1980
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1980pepi...22..155k&link_type=abstract
Physics of the Earth and Planetary Interiors, Volume 22, Issue 2, p. 155-161.
Physics
3
Scientific paper
Temperatures in the lower mantle of the Earth are estimated from the observed Q distribution. A thermal boundary-layer where temperatures rise rapidly is found at the base of the mantle, corresponding to the low Q zone described by Anderson and Hart (1978a,b). The existence of this thermal boundary layer indicates that the lower mantle participates in convection, and also that some of the energy driving the convection is coming from the core.
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