Field investigations in the Ketilidian rocks of the Nanortalik–Tasermiut region

Abstract

Before finishing the compilation of the anortalik sheet it had become necessary to check several things. Because of bad ice conditions during the summers of 1968 and 1969 it was only possibie to visit the area between Tasermiut fjord and the northwestern boundary of the Ketilidian sedimentary basin with the old reactivated basement in this part of Greenland, situated along Søndre Sermilik Gord and across the north-westernmost part of Sermersôq.