f Rift structure in Barents Sea from new interpretation of deep seismic sounding (DSS) data

The traveltime curves along the Barents Sea D S profile (materiels of the Institutes of Oceanology and Earth Physics of the USSR [1]) have been interpreted on the base of twodimentiónal velocity model. This profile 680 km long was stretched in the southeastern part of the Barents Sea from the costline to the north of the Rybachiy Peninsula in the direction of the Franz Josef Land and situated within the rear part of passive continental Barents Sea margin.