A PECULIAR BELT OF OBLIQUE FAULTING 6i 



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the flanks of the domes, while at the same time it tends to give 

 the observed slopes to the fault planes. 



This peculiar belt of oblique faulting is therefore attributed to 

 the eastward movement of the southern portion of the region rela- 

 tive to the northern, together with the local torsion and incidental 

 tension developed by the doming process. 



