the Thermal stream, capacity of a bark. A thermal stream and vertical movement

you are: the Thermal stream, capacity of a bark

Communication between a thermal stream and modern vertical movements

The Subsequent analysis has been carried out on initial cards with the interpolated values of a thermal stream and to cards of modern vertical movements where values have been averaged for trapezes of a geographical grid with dvuhgradusnym an interval. The studied area is limited 6 and 66 ° century d. And 38 and 70 ° with. sh. As the general number of measurements makes only nearby 500, the grid formed in such a way, is rare enough for the extensive studied areas, hence, in many cases it is impossible to display completely the temperature and dynamic conditions existing in separate elements of geological structure.

In some works results appear non-comparable, therefore it is possible to draw a conclusion on impossibility of realisation of the simultaneous analysis of all these parametres for such extensive area. Therefore it was necessary to divide all area into territories which differ from each other mainly on geological or tectonic properties.

These territories:

) Scandinavia,

) platform areas of Average Europe,

) the Alpine area,

) the Balkan region,

) Sredne-Russian height,

) the Caucasian region,

) North Russian lowland to the West from the Ural mountains,

) the north and the northwest of the Caspian region, East European (Russian) a platform (as a whole), the East European platform (to the north from Moscow), the Czech file, Karpatsky region.