the Thermal stream, capacity of a bark. The Caucasian region

you are: the Thermal stream, capacity of a bark

After such selection there are areas e and z in which dependence between a thermal stream and vertical movements, apparently, is rather probable. It is remarkable, that these areas incorporate with each other, i.e. The Caucasian region with the lowland adjoining it from the north. Dependence between both investigated parametres can be characterised in this case by changes of +0,15 mm/year on 1 мВт/м2. The Alpine and Karpatsky regions differ in low factor of correlation: this size varies there on 0,05 mm/year at change of a thermal stream on 1 мВт/м2. As repeated levelling does not cover high-mountainous sites, it is supposed, that speed of a raising actually will be a little above. Thus, the given value of change V and Q can even exceed the allocated twice. Probably, that in separate areas of platform areas the correlation factor is higher and corresponds to average change-0,05 mm/year on 1 мВт/м2. The difference in signs for respective alteration in vertical movements on unit of a thermal stream sufficiently characterises difference of platform areas from young orogenov.