the Field of a thermal stream in territory gdr. Anomalies of a thermal stream in gdr

you are: the Field of a thermal stream in territory gdr

In territory of GDR the thermal stream is estimated on 348 stations representing in most cases boreholes. The statistics is that:

Position of stations of measurement of a thermal stream, distribution of a thermal stream and the simplified geological structure of territory of GDR. Stations are concentrated in northern part of the country and around Tjuringsky pool. Here isolines are spent quite confidently. The territory of GDR can tektonicheski be divided on two bodies, and the border crosses the country in direction ZSZ - VJUV (' the median-German main break '). The area to the north from this zone of a break is a part of the Sredne-European sedimentary pool stretched from the east of Poland through GDR and Germany to the central area of the North Sea Capacity of not folded sedimentary cover here increases more than to 6 km. Raising Ringkyobing-Fjun and its east-southeast continuation at island Rjugen represent North country of this pool. The sedimentary trough valley - the Danish-Polish deflection - separates raising Ringkyobing-Fjun from dokembrijskogo the Baltic board in the north.

The Field of a thermal stream in northern part of GDR is characterised by several basic geothermal features:

The isoline in 60 мВт/м2 passes approximately in parallel southern edge of the Sredne-European sedimentary pool, showing to that the general fall of a thermal stream to the south;

In the central part of GDR anomaly of a high thermal stream is stretched from an eastern frontier of GDR to the river of Elba in the west. Crossing area of Berlin, this anomaly is the part of larger anomaly of a thermal stream extending from England through Average Europe to southeast Poland;

To the east from Berlin this shirotnaja anomaly branches: one anomaly of a high thermal stream departs in a northwest direction to coast of Baltic sea, and values of a thermal stream raise more than to 90 мВт/м2;

Along the western border of GDR narrow anomaly of a high thermal stream northeast prostiranpja is traced; in the south this anomaly proceeds on territory of Germany, and it is supposed, that it is a part of anomalies of a zone Mediterranean sea - Myosa. The nature of these anomalies of a thermal stream is not quite clear yet. It is possible to admit existence konvektivnogo teploperenosa along zones of deep breaks, but some influence could render and lateralnye variations radioactive teplogeneratsii in earth crust. The southern part of GDR concerns to gertsinskomu to a folded belt. Crystal and metamorficheskie breeds leave on a surface or are covered by a sedimentary cover (capacity to 1000 verhnekamennougolnogo Triassic age.