Weides, Simon; Majorowicz, Jacek - In: Energies 7 (2014) 4, pp. 2573-2594
Heat flow and geothermal gradient of the sedimentary succession of the Western Canada Sedimentary Basin (WCSB) are mapped based on a large thermal database. Heat flow in the deep part of the basin varies from 30 mW/m<sup>2</sup> in the south to high 100 mW/m<sup>2</sup> in the north. As permeable strata are required...