GRRAT SERPENTINE-BELT OF NEW SOUTH WALES, V., 



illustrate it here. Again, lateral injections and explosions 

 within unconsolidated sediments of the character we are con- 

 sidering, would be accompanied by more or less sliding of the 

 lamellse over one another, which would result in the tearing up 



.•OA. 



of the lamellse, and their injection into one another. This is 

 particularly well shown when black carbonaceous layers alternate 

 with white tu£F. A specimen of this is illustrated by Text- 

 figure 11, Again, the small convulsions caused by the ejection 



