the Thermal stream in danii. Boreholes

you are: the Thermal stream in danii

Boreholes Волдум-1, Квольс-1, Скиве-1 settle down over deep structures of hydrochloric pillows or is very close from them (depth to salt nearby 3000). We have subtracted positive influence of hydrochloric structures on value of temperature and a thermal stream a method of two-dimensional final differences on numerical models of the anomalies caused by deposits of salt just as it is made in work. Values of a thermal stream for chinks Voldum, Kvols and Skive decrease thus accordingly on 7,5 and 3 mVt/me. Relief influence in this case can be neglected.

It is considered, that paleoklimaticheskie variations essentially influence values of a thermal stream. Effect of possible climatic amendments. The model And contains unique temperature jump - increase on 8 To for last 10 000 years. Model In - more difficult function for widths 40-60 °. During last freezing Denmark settled down on border with the Fennoskandsky ice board. In Denmark otstupanie a glacier has begun about 16 000-17 000 years ago. The increase in temperature from 0 °s to present 8 °s communicates mainly with sharp warming, an event about 10 Open Companies of years back (the beginning of the postglacial period).