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The only deep temperature measurements were in the HDR boreholes at Rosemanowas quarry.
Analysing the calculated 3D thermal field, different thermal effects can be recognized affecting the deep temperature distribution in the Molasse Basin area.
Given the mentioned limitations, the results nevertheless indicate that assuming conductive heat transport as the first-order control for the thermal field is valid and give first-order estimates of deep temperature variations.
One other project investigating the deep temperature distribution in the European Molasse Basin is the project GeotIS (Geothermal Information System; Schulz et al. 2009; Agemar et al. 2012, 2014a, b) conducted by the Leibniz Institute for Applied Geophysics LIAGG) in Germany.
The sampling procedure, including 5 seconds of filtering on a 0.45 µm filter was chosen as being extensively used in microorganisms studies [33] and as shown to be superior in comparison with deep temperature quenching [34].
Superficial and deep temperature changes depend on the application procedure, initial temperature, application time, application area, and location [ 33].
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Hydraulically less conductive Folded Molasse Sediments would lead to higher deep temperatures at the Alpine front, but lower temperatures in the rest of the basin.
It should be noted that the basement heat production, A B, was the heat production to 5 km depth for temperature depth slices to 5000 m and the heat production to 10 km depth for deeper temperature depth slices.
Moreover, Agemar et al. (2012) recommend a careful treatment of the deeper temperature estimates of GeotIS (StMWIT 2010), since the data base decreased with depth and hence possible local thermal effects may not be considered in the temperature interpolation.
As you go deeper, temperatures go up but so do costs.
A simple weighed combination of box temperature of the device and 14 cm deeper temperatures can provide a useful level of Wenner compensation.
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