Abstract
Abstract Marine seismic reflection profiles across McMurdo Sound have been interpreted using the results of the MSSTS-1 drillhole. The data show that the sedimentary sequence under McMurdo Sound is mainly early Tertiary or older in age, with the post-Eocene section less than 800 m thick. The seismic records show major erosion of the younger sediments, possibly by slumping, from the western slope into the deeper water of McMurdo Sound.
Full Text 
Sign-in/Register to access full text options
Sign-in/Register to access full text options 
Published version (
Free)
Free) 
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
