the Analysis of a superficial thermal stream. Features of a thermal field evropy

you are: the Analysis of a superficial thermal stream

The main features of a thermal field of Europe - low values of a thermal stream on the East European platform and raised in southern and central parts of continent.

Considering such considerable heterogeneity, it is necessary to expect considerable distinctions in a geothermal mode of both areas that leads to a conclusion about existence lateralnyh variations physical and reologicheskih properties of the top cloak. Special interest is represented by distinctions of density, elastic properties (speed R - and S-waves) and elektroprovodnosti.

As the first step dependence of temperature on depth along a profile stretched from Corsica to Leningrad has been calculated.

For the further interpretation and as a basis following questions are most interesting to geodynamic conclusions: are how much great in the top cloak lateralnye heterogeneity of distribution of temperature and heat sources, on what depth these can extend heterogeneity and as it influences viscosity mantijnogo a material.