Abstract:Bathymetry and single seismic reflection methods were used to study the seafloor inhomogeneities in the Norwegian-Greenland region. North of the Mohns Ridge we have identified nearly east-west trending morphostructures (MS) in seafloor relief, which are horst ridges separated by troughs, and have provided their characteristics. We carried out a seismostratigraphic analysis to study the structure of the Cenozoic sedimentary cover and the conditions that existed during its formation. We showed that these seafloo… Show more
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