Abstract
The geological and geophysical materials on distribution of the glaciations and sea transgressions that occurred in the last 140 thousand years have been analyzed considering glacio-eustatic transgressions and position of the Ocean level. While the glaciation degraded and the rise of the continent was less than the rise of the sea level, transgressions took place. The most probable areas of glaciation distribution during marine isotope stages (MIS) and sub-stages 6, 5b, d, 4, 2 have been reconstructed. It is shown that the sea transgressions related to glaciations took place in MIS 5e, d, 2 and 1.
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.
