the Thermal stream, capacity of a bark

The Thermal stream, capacity of a bark and modern vertical movements

P.Vyskochil

The Summary. In article in a preliminary order conclusions about communication between a thermal stream and (or) depth of section Mohorovnchicha and the modern vertical movements measured by means of repeated levelling are considered. Some areas of Average and the Eastern Europe were studied, and the data received from the International centre on studying of modern movements of earth crust were used. For convenience of the analysis all studied area has been divided into the areas possessing whenever possible homogeneous tectonic features. As it is possible to conclude from the received results, areas of young folded belts are characterised by more intensive vertical movements and the raised values of a thermal stream. In areas of platform type there is an inverse relationship: immersing with increase in a thermal stream prevails. Between depth of section Mohorovnchicha and intensity of vertical movements dependence less accurate.

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