the Thermal stream in danii. A thermal stream and deep temperatures

you are: the Thermal stream in danii

The thermal stream and deep temperatures in Denmark should be studied in close interrelation with tectonic conditions in region. The area of Denmark occupies a northeast part of the North Sea or a northwest part of the European sedimentary pool, which is limited from Scandinavian peninsula Fennoskandsky (or Baltic) by a board. Apparently, in sedimentary pool a thermal stream considerably above, than on the next board (see the card of a thermal stream enclosed to this book). The Fennoskandsky board, as well as other boards, basically is characterised by low values of a thermal stream - from 40 to 50 мВт/м2 while in a hollow of the North Sea the thermal stream makes, possibly, from 60 to 80 мВт/м2. According to modelling calculations of temperatures of a bark and the tops of a cloak and a field of a thermal stream of this transitive zone, the most probable had been recognised that distinctions in a superficial thermal stream are caused by different thermal streams from a cloak.

And temperature interest to studying of a thermal stream Recently has considerably increased in Denmark thanks to presence of geothermal resources low entalpii which can be maintained.