M = 



[("„)• "- 



*]s/ 



/ = 

 s 



V p 





V 

 P _ 







/l.O-a 





V 

 s 



V 0.5 - a 





Additionally: 



K^ 



sat. 



I p(v y is +3] 



sat. L V py sat. J 



(6) 



(7) 



(8) 



(9) 



P- 



X = K - 2/3 ^ (10) 



Where, in addition to notations of (1) to (4): 

 a - Poisson's Ratio 



V - velocity of the shear wave 

 s 



E = Young's Modulus 

 X = Lame's Constant 



GEOACOUSTIC MODEL NO. 2: 

 EXPERIMENTAL MOHOLE (GUADALUPE SITE)* 



The sediments cored by the Experimental Mohole 

 Project from the deep-sea floor east of Guadalupe Island, 

 Mexico, during March and April 1961, were divided among 

 a large number of institutions and individuals for various 



* The substance of this section has been published in 

 reference 24. 



25 



