Figure 5. Equilibrium temperatures vs. depth from the ADARA and WSTP temperature sensors tool runs (data from Comas, Zahn, Klaus, et al., 1996). The seafloor temperature, T0 , and the geothermal gradient, G, are calculated from a linear regression of the data.

Figure 5. Equilibrium temperatures vs. depth from the ADARA and WSTP temperature sensors tool runs (data from Comas, Zahn, Klaus, et al., 1996). The seafloor temperature, T₀ , and the geothermal gradient, G, are calculated from a linear regression of the data.