Lower Palaeozoic carbonates in eastern North Greenland, and the demise of the 'Sæfaxi Elv nappe'

The principal aim of the authors was to document the stratigraphy and structure of Ordovician and Lower Silurian sediments in a c. 5000 km2 area in southern Kronprins Christian Land and westernmost Lambert Land, and estimate the palaeogeographical position of Greenland in relation to the areas surrounding the lapetus Ocean.