the Thermal stream in danii

Deep temperatures and estimations of a thermal stream in Denmark

H. Balling

The Summary. Data on a deep temperature field of Denmark are almost entirely received on the measurements executed in chinks for an oil recovery and gas and given scientists by the oil companies. The generalised geoisotherms have been constructed for various levels to depth of 3000 m where temperatures from 70 to 100 ° by S.Samye heats have been found out observed on the areas to which there correspond the deepest sites of sedimentary pools. Estimations of a thermal stream in six areas are resulted, five of which are in the central part of the Danish site of a hollow of the North Sea (the Danish subpool) in northern Jutland. A thermal stream here from 60 to 65 мВт/м2, around Copenhagen - nearby 45 мВт/м2. Apparently, climatic amendments should raise these values on 10-15 мВт/м2. Possibly, deep temperatures and a thermal stream decrease in a direction from deep sedimentary hollows to dokembrijskim to structures of raising Ringkyobing-Fjun and the Fennoskandsky board. The highest korovye temperatures are counted up for the Danish subpool in northern Jutland, where a sedimentary layer the most powerful. At the basis of thicknesses capacity about 10 000 m receives temperatures from 250 to 300 ° S

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