QUANTITATIVE STUDY OF SEA-LEVEL CHANGES

This paper emphasizes the differences and relations among relative sea-level changes,eustatic changes and water depths. It is proved that compaction can be neglected While calculating sea-level changes with the stratigraphic thickness. It is also be demonstrated that in along time interval the changes of water depth might be consistent with sea-level changes. Atlast a method for the construction of curves of relative sea-level changes and eustatic changesare presented.