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Mean value is 65 mW/m2 over continental crust and 101 mW/m2 over oceanic crust.


0.9 and 105.4 mW/m2.[1]

See also


Physics / Thermodynamics / Heat Transfer / Heat flow / Heat Flux


Reference


  Davies, J. H., & Davies, D. R. (2010). Earth's surface heat flux. Solid Earth, 1(1), 5–24.

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