RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES3002, doi:10.2205/2017ES000598, 2017

Figure 21. A seismostratigraphic interpretation of the time section for V2304.1 (the position is shown in Figure 1). LB-1 and LB-2 are seismic units of Cenozoic sediments in the Lofoten basin; I–III denote subunits of LB-2; $H_{\mbox{sed}}$ is sediment thickness; the circle with a dot marks turn in the line. The arrows inside the seismic units fit the sedimentary layers (for explanations see text).

 
Citation: Usenko S. V., A. N. Boyko, T. V. Prokhorova (2017), Seafloor relief inhomogeneities and the tectonics of the Greenland-Lofoten Basin in the North Atlantic, Russ. J. Earth Sci., 17, ES3002, doi:10.2205/2017ES000598.
 

Copyright 2017 by the Geophysical Center RAS.