Geothermal data on bolgarii. A picture rodopskogo a file

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The picture of the Rodopsky file is extremely difficult. Considerable distinctions in development of a relief and orientation of folded structures and breaks are marked. Structures of the western Rodopsky block have mainly meridionalnoe and a northwest direction while east Rhodope are focused shirotno. The western block basically is connected with system of breaks Strumy, east - with system of breaks of Maritsa. The same breaks define a general plan of folded structures of a file. Depressions in east block are wider in comparison with narrow structures grabenov, tracked to the West from depression Brazigovo - Dospat. There are also distinctions in development magmatizma both blocks in a neogene. In east block meet treshchinovatye basalts which are not present in the western block.

These tectonic features define various thermal modes of a file in separate blocks. The thermal field of the western Rhodope is not studied. Presence of thermomineral waters allows to draw some conclusions. In the central Rodopsky anticline thermal characteristics, as a rule, appear above in areas of a svintsovo-zinc mineralization. The raised thermal stream is connected with processes of strong crushing and activization in poslepaleogenovyj the period. On character of a thermal field the main influence is rendered by aforementioned depressions with verhnepaleogenovymi and neogenovymi - chetvertichnymi deposits. Some were formed of these depressions over ancient negative structures, such, as east Rhodope, Brazigovo - Dospat, the Top Thrace etc.