the Thermal stream in velikobritanii. The analysis of results

you are: the Thermal stream in velikobritanii

From materials follows, that there are two belts in which values of a thermal stream as a whole exceed 60 мВт/м2. More southern of them passes from southwest England where are bared granity, characterised big teplogeneratsiej, in east direction along southern coast to Dorset and Hampshire. This southern belt is located within area which has been deformed and is weak metamorfizovana as is on northern termination gertsinskogo a folded belt of Europe. Northern belt concerning the big thermal streams is stretched from Lincolnshire on the northwest to Lake district. In most

Lake district (in which it is not spent measurements of a thermal stream) and under Northern Penninami deformed slabometamorfizovannyj nizhnepaleozojsky the base is broken through by small granite rods nizhnedevonskogo age.

Richardson and Oksburg have shown, that between values of a thermal stream and teplogeneratsiej breeds of the base in the Great Britain there is a linear dependence of such type as it is described in work. According to its authors, Pollack and CHepmena, this correlation is applicable and to areas where the base is combined granitami, and to those districts where it includes poorly-perekristallizovannye oblomochnye breeds. Presence of such correlation testifies that belts of a high and low thermal stream are belts higher and lower teplogeneratsii breeds of earth crust.

Apropos granitov southwest England Tammemagi and Uajldonom other point of view has been put forward; they have assumed, that exclusively big anomaly of a thermal stream over these bodies can be caused konvektivnym teploperenosom, operating on depth in limits plutonov.

Thanks. We thank Bikla, Martin and Right for article discussion. Richardson has kindly given us algorithm for transition from national system of co-ordinates of the Great Britain to system of polar co-ordinates.