the Thermal stream in danii. Data of deep seismic sounding

you are: the Thermal stream in danii

Data of deep seismic sounding in Denmark have been partially interpreted and discussed Hirshleberom. Models give normal distribution for continents korovyh speeds of R-waves with the values close to 6 km/s in the uppermost part dokembrijskogo of the crystal base under a sedimentary cover. On depth from 18 to 28 km there can be a jump of speed from 6,4-6,5 to 6,7-6,8 km/s. Models Hirshlebera give to speed of 7,2 and 7,35 km/s at the basis of a bark and 8,0 and 8,05 km/s under section Mohorovichicha which depth makes in the Danish subpool of northern Jutland about 32 km. Under raising Ringkyobing-Fjun capacity of a bark can be a little above, an order of 35 km. In sedimentary pool capacity of a bark is less, than in the next Fennoskandsky board. The Fennoskandsky board on a sea level has average capacity of a bark of an order of 39 km, and southern Norway with capacity of a bark about 32 km is an exception.