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Fig. 8 | Geothermal Energy

Fig. 8

From: Curie point depth, thermal gradient, and heat flow in the Colombian Caribbean (northwestern South America)

Fig. 8

Geothermal gradient comparison for the offshore part of the Colombian-Caribbean domain. Red lines represent the geothermal gradient calculated by the centroid-fractal method, the blue lines correspond to the BSR-based geothermal gradients. The broken black lines represent centroid-fractal method-based gradients corrected by the mean difference between both types of data. Figures next to right of the lines are the difference between the two types of gradients. Where no broken black line is present, the difference between the gradients is equal to zero. Numbers in parentheses, at lower left corners, identify seismic line (see location in Fig. 2)

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