geotermija vengrii. The Pannonsky hollow

you are: geotermija vengrii

Judging by the review resulted above, in the Pannonsky hollow there is a difficult system of circulation. Thanks to calculations on simple model and to field researches it was possible to show, that the field temperaturoprovodnosti can test appreciable indignations (to 100%), first, in vicinities gidrogeologicheski active breaks in mesozoic karbonatnyh breeds, and secondly, at litologicheskih windows in verhnepannonskih vodonosnyh horizons. In chetvertichnyh layers and in verhnepannonskom a complex it is necessary to expect less considerable indignations, to 30%, and smaller changes of temperature, to 15%. Other formations usually do not become complicated water circulation.