540 



JOSEPH BARRELL 



5K-.02i 



A 



t)' 



DeflecHon 

 residuals and 

 gravity anomalies 



M 



X$ 



+5-1 



<>• 



F(j componenhs s-, 



of deflechon residuals 



'-S -^ 



F;< coTnponen|-s 



of deflechion residuals 



Scale For residuals'^ 



10" 



100 o 

 liiiiiiiiii 



' ■ ■ ■ ' I ' ■ ■ ' 



Scale for distances 

 I ' I 



sooKm 

 J I 



Fig. 12.— Residuals of Solution H and gravity anomalies in Texas, Oklahoma, 

 and Kansas, with the interpretation of the outstanding masses in terms of equivalent 

 spheres. 



