the Field of a thermal stream in territory gdr. Stations of a thermal stream

you are: the Field of a thermal stream in territory gdr

Stations of a thermal stream concentrate in two areas: in Tjuringsky pool and in Erzgebirge. Out of these areas the thermal stream can be estimated only in general (within the Luzitansky plate and in the central Saxony), but as a whole it, apparently, does not exceed 60-65 мВт/м2.

Distribution of a thermal stream in Tjuringsky pool is in detail discussed in works. The small anomalies of a thermal stream connected with a relief crystal or metamorficheskogo of the base have been allocated some. The raised values of a thermal stream near to the western border of GDR otnosjatsjak anomalies Verhnerejnsky grabena - an Alto-mark, having North northeast prodeleting.

The Most considerable geothermal anomalies in a southern part of GDR settle down around Erzgebirge, crossing here border with Czechoslovakia.

Taking into consideration data about a thermal stream across Czechoslovakia, it is impossible to consider positive anomaly of a thermal stream of Erzgebirge local; it settles down on crossing of two regional anomalies of a thermal stream: one of them passes in a northeast direction along the western border of the Czech file, another - in a northwest direction (the Labsky line, on CHermaku).

Both anomalies are connected with systems of deep breaks. From modelling calculations of distribution of temperature with depth follows, that the temperature on border a bark - a cloak varies approximately from 800 to 850 °