相对海平面上升已成为中国沿海地区海洋地质环境灾害之一。
Relative sea level rise has become one of the geological environmental hazards in the coastal areas in China.
基准面的变化是构造、气候的函数，对于地史时期的滨海盆地，基准面就是相对海平面。
Base level was the function of tectonic movements and climate circles, and base level for coastal basin in geological history was relative sea level.
对凝缩段的识别不仅是认识层序结构的关键，而且对分析地质历史时期全球相对海平面变化至关重要。
Identification of condensed section is not only the key to understanding of sequence structure, but also critical to analysis of global relative sea level changes during geologic history.
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