Geothermal data on bolgarii. A tectonic zone Balkan forlanda

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The tectonic zone Balkan forlanda at investigated levels differs on thermal parametres from geothermal characteristics of the Mizijsky plate a little.

The Alpine floors of western and east parts of the Balkan folded zone were generated in various conditions. The western part was steadier and more raised throughout all period of time in comparison with central and east parts. Accordingly the lowest thermal stream should be in the west.

Because of complexity of geological structure of the south of Bulgaria and limitation of temperature data the detailed analysis of communication of geothermal anomalies and geological structure is difficult enough. Nevertheless in a zone of Balkan mountains which, it agree Bonchevu, are stretched to the West from a valley of the river Timok and to the east up to Black sea, the tendency of rise in temperature and a gradient from the West on the east is marked. It, apparently, is connected with the big distinctions in geological structures of western and east zones of the Balkans.