the Thermal stream and an arrangement of ruptures. The East European platform

you are: the Thermal stream and an arrangement of ruptures

The East European platform. Low and very low values of a thermal stream are typical for this area. Average value nearby 40 мВт/м2, makes a standard deviation 9,8 мВт/м2, that specifies in existence only the small indignations of a thermal field connected with the local reasons, such, as systems of ruptures with konvektivnym teploperenosom. Really, in all territory of the East European platform of anomaly of a thermal stream have very flat form and with existing systems of ruptures it is not found out their any correlation, even on the areas with high density of geothermal supervision (for example, in Ukraine).

It means, that systems of breaks, in particular character and age of ruptures, do not influence a thermal mode so.