Abstract
In this paper, we calculated the travel time of the transverse waves reflected at the boundary of the earth's nucleus situated at the depth of 2900 km. using the velocities of the seismic waves obtained by B. Gutenberg and compared this with the ScS phase revealed on the seismograms of some deep focus earthequakes. Thus we drew the conclusion that the velocities shown by Gutenberg seem to be a little too great in the earth crust.
Sign-in/Register to access full text options 
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 callMore From: Journal of the Meteorological Society of Japan. Ser. II
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
