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, This study uses TNO's in-house thermal modeller, Basin 3D, to create a steady state
This is the a priori model and starts from a lithological geometrical model. The a priori thermal properties are then populated for each grid cell, to give k (z), a collection of 1D thermal conductivity profiles (W m -1 K -1 ) as a function of depth for the sediments, upper crust, lower crust and lithospheric mantle. The bulk matrix conductivity, k m, 2009. ,
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This is particularly relevant for producing geothermal energy in non-volcanic areas, which is not yet common due to the difficulties in predicting optimum well locations in such areas. Reducing exploration and production risk in non-volcanic areas could largely increase the global potential for geothermal energy, and take it beyond its current status as a resource restricted to volcanic areas. 4.1. Acknowledgements Research presented in this chapter was conducted as part of an industrial secondment at TNO, Utrecht, under the SUBITOP ITN and in collaboration with Utrecht University. This falls under the European Union's EU Framework Programme for Research and Innovation Horizon 2020 under Grant Agreement No 674899. I am very grateful for the hospitality and conviviality the Utrecht team showed me during my secondment, and for the additional help and support they extended afterwards in completing the chapter, who emphasised that tectonic studies can aid in both predicting and producing geothermal energy (refer to chapter, 2010. ,
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