Age and correlation of supracrustal rocks in the Frederikshåbs Isblink area

Abstract

Eight weeks field work was spent in the Frederikshåbs Isblink area as a continuation to the investigations carried out in 1967. Half the time was used to further the work on Dalagers Nunatakker and half was spent on the gneisses and supracrustal rocks north of the Isblink in an attempt at correlation across the Isblink between the gneiss-amphibolite complex of the Frederikshåb area (see Jensen, 1966) and the Ravns Storø region (Windley et al., 1966; Windley, 1968).