Temperature a gradient in ispanii. An earth crust structure

you are: Temperature a gradient in ispanii

Under the program of the International geodynamic project measurements along several profiles GSZ have been spent. Preliminary results of these measurements in aggregate with gravimetricheskimi data have given the first information on an earth crust structure in territory of Spain. Spanish Meseta, occupying the most part of the central area of peninsula, it is characterised by the most powerful bark, and section Mohorovichicha is there on depth of 36 km. In this area negative anomalies Bug are observed, as a rule. From the southeast and the southwest the central part of peninsula is bordered with area with rather thin bark to which there correspond positive anomalies Bug. Section Mohorovichicha settles down on depth of 31 km in Almeria and only 27 km around Cartagena.

If the specified data on capacity of earth crust to compare with a picture of distribution of a thermal stream there is obvious a negative correlation between these parametres. The maximum values of a thermal stream were observed in the areas of a thin bark characterised by positive anomalies Bug, near to the Mediterranean coast, and, on the contrary, the weakest geothermal activity corresponds to a powerful bark in the central part of the country.