geotermija vengrii. Sizes shtegeny

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Sizes SHtegeny regularly more low, and the difference increases with depth. This results from the fact that on cards SHtegeny temperatures of a face of chinks, which regularly more low, than equilibrium values prevail. On the other hand, values Boldizhara, apparently, are overestimated. In particular, increase in average heat conductivity with depth in the range of 0-3000 m much more, than those of 13% on which as assumed Boldizhar, the temperature gradient decreases with depth. But as outlines of isolines on cards are mutually similar and well correlate with thickness of a sedimentary layer of a hollow, it is possible to consider these cards authentic for ' relative ' estimations.