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Fig. 11 | Geothermal Energy

Fig. 11

From: Geothermal resource assessment of remote sedimentary basins with sparse data: lessons learned from Anticosti Island, Canada

Fig. 11

Temperature sensitivity with respect to thermal parameters considered computing analytical 1D profiles, using DZ017 well. Impact of a lithology from the synthetic logs of other zones are applied to the calculation of the thermal conductivity and heat generation rate in the sedimentary thermal units; b the thermal conductivity assigned to the lithologies of sedimentary thermal units; c the thermal conductivity assigned to the Basement thermal unit; d heat generation rate assigned to the entire sedimentary basin; e BHT corrections, and f mantle heat flux were evaluated separately

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