part 1] AND ASSOCIATED ROCKS OF MOZAMBIQUE. 67 



VI. The Geaxulitic Granites and Pegmatites. 



The later granites of Mozambique never occur in large intru- 

 sions such as have been described from other African areas. 



Occasionally they form the cores of some of the inselberg peaks, 

 and, although they may resemble very closely the granulitic facies 

 of parts of the older gneissose granites, their relative age can 



f2 



