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- W4381848610 endingPage "144" @default.
- W4381848610 startingPage "133" @default.
- W4381848610 abstract "The thermal conductivity of the minerals in the vicinity of the Earth's core-mantle boundary (CMB) affects the structure and thickness of the thermal boundary layer of the mantle, which constrains the core cooling rate and Earth's total heat budget. Herein, we review recent experimental and theoretical studies examining the thermal conductivity of the Earth's lower mantle. Existing results of our thermal conductivity measurements were combined to construct self-consistent models for the lowermost mantle conductivity. We used these models to conduct simulations of the temperature profiles at the base of the mantle and the CMB heat flux. The averaged global CMB heat flow is estimated to be approximately 10 TW, which is in line with traditional estimates. The total heat flow of approximately 10 TW with large regional flux variations promotes interaction and co-evolution of the core and mantle." @default.
- W4381848610 created "2023-06-25" @default.
- W4381848610 creator A5013685986 @default.
- W4381848610 creator A5035391577 @default.
- W4381848610 date "2023-06-23" @default.
- W4381848610 modified "2023-10-17" @default.
- W4381848610 title "Heat Flow from the Earth's Core Inferred from Experimentally Determined Thermal Conductivity of the Deep Lower Mantle" @default.
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- W4381848610 doi "https://doi.org/10.1002/9781119526919.ch8" @default.