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Sagot :
The rate of silicate melting and volcanism will be governed by heat production, which will also affect the mantle's temperature. Thus, a major force behind the dynamics of rocky planets is the creation of radiogenic heat in the mantle. In turn, dynamics has an impact on planetary habitability.
In order to accurately estimate lithospheric temperatures and comprehend processes associated to the thermal evolution of the Earth, radiogenic heat production is a physical quantity that is essential.
Mantle convection is strengthened and the mean mantle temperature is raised as a result of radiogenic heat production. The thermal lithosphere becomes thinner as a result of the warmer mantle.
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