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- W2246015269 abstract "The thermal evolution of the mantle is controlled by mantle convection, whose operation is strongly influenced by the marked temperature dependence of the viscosity of mantle materials. The heat transported by convection can be represented through a simplified ‘parametrized’ formula. Typical calculations yield an early transient phase lasting about 0.5 Ga, in which excess heat from Earth's accretion is removed, and a later phase in which the thermal state is controlled by slowly decaying internal radioactivity. Geological evidence is approximately compatible with this kind of history. However, the inferred rate of heating is larger than current cosmochemical estimates of Earth's complement of radioactive heat sources. It is not yet clear whether plate tectonics operated in the first half of Earth history, so the early evolution is subject to substantial modification." @default.
- W2246015269 created "2016-06-24" @default.
- W2246015269 creator A5003805866 @default.
- W2246015269 date "2007-01-01" @default.
- W2246015269 modified "2023-09-25" @default.
- W2246015269 title "Thermal Evolution of the Mantle" @default.
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- W2246015269 doi "https://doi.org/10.1016/b978-044452748-6.00145-0" @default.
- W2246015269 hasPublicationYear "2007" @default.
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