Interpretation of field observations in the southern part of the Ilímaussaq intrusion, South Greenland

Abstract

During the 1971 field work mapplng at the scale of 1: 10 000 was continued in the area of Kangerdluarssuk fjord (see Demin, 1971). The most important field observations arising from the mapping are interpreted below. These notes should be viewed in the light of the earlier work on naujaite and lujavrites in the Ilimaussaq intrusion (see references in the text and Ferguson, 1970).