the Thermal stream, capacity of a bark. Conclusions

you are: the Thermal stream, capacity of a bark

Some parametres which should be set in model, difficultly estimate with necessary confidence. It is possible to imagine, that on the big depths the heat conductivity factor has higher values or that on a bark is necessary smaller percent of the general generation of heat. Certainly, it will affect absolute values of a field of temperatures, but will not change an influence overall picture lateralnyh variations. Therefore it is possible, possibly to consider proved following conclusions:

Large variations of a thermal stream are caused in Europe mainly by non-uniform distribution of sources of heat in earth crust;

lateralnye temperature variations can extend to depths more than 500 km;

Deep to heterogeneity of placing of sources of heat do not render considerable influence on a superficial thermal stream.