晚冰期（late glacial）是指晚更新世末次冰期的结束时期，约从距今15000年（或14000年）前至10000 年前。北半球大陆冰盖迅速消退，世界海平面开始回升，植被带逐渐向高纬度方向推移。
The main reason of the interruption for mirabilite deposition may be transient warming events. Therefore,the rhythm deposition formation of mirabilite-silt-mirabilite indicated the periodic changes of temperature during the late glacial and the Younger Dryas.
芒硝沉积中的淤泥细线为短暂升温标志,芒硝-淤泥-芒硝的沉积韵律揭示了晚冰期和新仙女木期气候的不稳定性和温度的周期性变化。
参考来源 - 河西走廊花海剖面晚冰期以来年代学及沉积特征研究·2,447,543篇论文数据，部分数据来源于NoteExpress
孢粉记录所反映的若尔盖地区晚冰期以来的气候演化与全球气候变化具有较好的可比性。
The climatic evolution since the late glacial epoch in the Zoigê area reflected by sporopollen records may be well correlated with the global climate change.
至晚冰期的年代地层序列和古气候环境，同时对沙山成因、古湖沼形成机制进行了深入探讨。
This paper, in detail, deals with the cause of formation of sand hill and formation mechanism of palaeolimnology.
本文从杭州湾地区末次冰期以来的地质背景入手，分析了该区晚第四纪地层层序、深切河谷形成和演化等。
This paper analyses the stratigraphic sequence of the Late Quaternary and formation and evolution of the incised valley in the Hangzhou Bay area, on the basis of the geological setting.
应用推荐