Figure 2.12. Steady-state thermal model.. This is a derivation of crustal geotherm based on a steady-state conduction model of the crust. Crustal parameters and boundary conditions are given in the model text. The solution attained is the one graphed in Figure 2.11. Use your mousewheel to zoom and mouse to pan to see details. If you would like a pdf copy of this derivation, click the download button.
