336 
NANANANNNVVVVVVVVVVWNANNAAAANAN ADDED AAA PDA LLLSLLALLARSE 
NAAA AAA AAA LAOAL AA PDALODALLLL УХА ИИ АА УИ 
70 60 50 40 30 20 10 о 10 20 30 40 50 
ee ee ait ll == 1 = i ne i D 1 J 
Fig. 31. Analyses of rocks of the unstratified part of the Ilimausak complex. 
A arfvedsonite-granite (analysis 1, р. 114); В nordmarkite (17); С augite-syenite (16);] D essexite (13). The vertical distances belween the rows 
have been chosen proportional to the differences between the silica percentages. 
