geotermija vengrii. Tektonofizika pannonskogo a maximum

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Tektonofizika the Pannonsky maximum of a thermal stream

We already saw, that only one hydrothermal circulation cannot explain high values of a thermal stream in the Pannonsky hollow. It is necessary to find the deep reasons which could explain rather homogeneous high thermal stream. This mechanism should be somehow connected with tektogenezom the Pannonsky hollow. In recently published works as the corresponding mechanism ascending movement of partially fused substance of a cloak - thermal mantijnyj diapir is offered.

The basic geophysical features of the Pannonsky hollow are More low listed:

1. The top part of a bark has normal capacity (17-19 km), and the bottom bark - thin (6-10 km).

2. Calculations on gravitational model show, that density of the top cloak in a hollow below norm.

3. The top edge of a layer of the lowered speeds of the top cloak is raised (60-70 km).

4. Delay of seismic waves - positive.

5. Vysokoelektroprovodnyj the layer of the top cloak is raised (45-65 km).

6. Calculations on thermal model testify that on depth of 60 km prevail temperatures 900-1600 °s and values of a thermal stream 40-60 мВт/м2.