the Thermal stream, capacity of a bark. Capacity of a bark

you are: the Thermal stream, capacity of a bark

Capacity of a bark and modern vertical movements

Communication between depth of section Mohorovnchicha (and modern vertical movements (V) investigated in precisely the same way, as well as in the previous case, and for the same subdistricts. In connection with that that for some areas of Europe of value of a thermal stream are known, while data about depth of section Mohorovnchicha are absent, representations about approximate convergence of these parametres are used. The analytical results received for separate areas, show communication between both parametres with the factor of correlation varying from 0,01 to 0,66. This result will be co-ordinated with the data received earlier. It is possible to assume, that deformations of a terrestrial surface are caused by deformations of the bottom border of the bark which in turn are exposed to dynamic influence of a cloak. Therefore there can be a communication between the form of section Mohorovnchicha and superficial deformations. Obviously, this communication by places will be implicit for two reasons: Comparison is spent between dynamic (deformation) and static (a relief of section Mohorovnchicha) elements and it is very probable, that vertical deformations are accompanied by the horizontal.

Some results showing communication between depth of section Mohorovnchicha and vertical movements, and also communication between a thermal stream and vertical movements. Regress lines are resulted for the values received in the Alpine area, the Caucasian region and for a data set for caucasus and Carpathians together. Results specify in dependence which is characterised by increase in a raising with increase in depth of section Mohorovnchicha and strengthening of a raising with increase of a thermal stream. On these data still it is impossible to tell with definiteness, this communication by result isostatic or lateralnyh horizontal movements is.