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Structure of a diffuse suture between Fennoscandia and Sarmatia in SE Poland based on interpretation of regional reflection seismic profiles supported by unsupervised clustering
(2021-03-31)
The Paleoproterozoic suture between Sarmatia and Fennoscandia (SFS), two major components of the
East European Craton, extends SW-ward from Russia through Belarus to SE Poland. The exact
character of this suture remains ...