Assume that a region of continental crust has a typical surface heat flux of 65 mW/m 2
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Assume that a region of continental crust has a typical surface heat flux of 65 mW/m2, crustal density of 2750 kg/m3, and typical crustal abundances of radioactive nuclides (as given in Table 20.6). If 60% of the surface heat flux comes from radioactivity in the upper crust, to what depth does this typical crustal composition extend?
Table 20.6
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