Abstract
The dispersion of fundamental-mode Rayleigh waves for several paths in Fennoscandia is consistent with the geological setting for the Baltic shield. Additional dispersion data indicate that the Barents Sea is a shield as well. The dispersion under the Baltic Sea is similar to the north-central United States, suggesting the extension of the mantle shield structure beneath the continental Paleozoic sedimentary cover.
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 callDisclaimer: 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.
