摘要
强调了水深、相对海平面变化与全球海平面（Ｅｕｓｔａｓｙ）变化的不同及相互关系。论证了应用实测地层厚度计算海平面变化时可以忽略压实作用，在较长的时间间隔内，水深的变化可能与海平面的变化一致。探讨了相对海平面变化和全球海平面变化曲线的建立方法。
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.
出处
《中国区域地质》
CSCD
1996年第1期75-82,共8页
Regional Geology of China
基金
国家攀登项目
地质行业基金
