Measurements of a thermal stream frg. A card of a thermal stream and its interpretation

you are: Measurements of a thermal stream frg

Many values settle down in the several limited areas whereas extensive sites are empty. It speaks mainly the purposes of investigation or distribution of corresponding lakes where can be used lake zondovaja technics. Therefore isolines of a thermal stream, represent only one of possible interpretations of a thermal stream and should be reconsidered, if there will be new data. To put isolines in borders of Federal Republic of Germany, values of a thermal stream, data Hurtigom and SHlosserom for GDR, CHermakom for Czechoslovakia both Henelem and TSotom for Austria are considered. Isolines in a southwest part Rhine grabena are based on values thermal-stream which were calculated at use of temperature gradients and prospective factor of heat conductivity 4-10-3 kal / (sm-to) which approximately corresponds to heat conductivity of tertiary deposits.

As to distribution of values of a thermal stream, it is represented, that correlation with large geological structures is very probable. The similar picture was already marked Hurtigom and SHlosserom. Values more low 60 мВт/м2 are found out mainly in sedimentary pool of Northern Germany. In molassovom the pool of Southern Germany executed by young deposits, values also, it is obvious, above, than in Northern Germany. It ' can be result Alpine orogeneza. Besides, it is impossible to ignore and possibility teploperenosa, caused by water migration at consolidation of deposits that, possibly, does not occur in the North German sedimentary pool. To mesozoic and Paleozoic structures there correspond values between 60 and 80 мВт/м2 with the tendency (statistically not confirmed) to fall of values in more ancient geological formations.