Abstract
Abstract Travel times for the seismic core waves, PKP, PKS, and SKS, were computed by integration along the travel paths. For this purpose the velocity distribution within the earth was broken into segments which were represented by continuous functions. Except for rays of grazing incidence to the outer core the times calculated for PKP and PKS are intermediate between the smoothed times given by Jeffreys and times based upon recent observed data. The times calculated for SKS are in fair agreement with the smoothed times given by Jeffreys.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Paper version not known
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a call
