地质学报（英文版）2000，Vol.74Issue(2)：266-272,7.
Evidence of the Pan-Lake Stage in the Period of 40- 28 ka B.P. on the Qinghai-Tibet Plateau
Evidence of the Pan-Lake Stage in the Period of 40- 28 ka B.P. on the Qinghai-Tibet Plateau
摘要
Abstract
The Qinghai-Tibet plateau is one of major saline lake regions in China, where saline lakes are widespread and constitute an important object of researches on the palaeoclimatic change in the region. On the basis of comprehensive investigations of the evolution of the lake's surface and sediments on the plateau, the authors have further demonstrated the existence of a pan-lake stage (river and lake flooding stage) on the Qinghai-Tibet plateau during the period of about 40+- 28 ka B.P. and analyzed the palaeoclimatic characteristics of the pan-lake period and relationships between the ancient monsoons and the uplift of the plateau since the beginning of the Quaternary.关键词
Qinghai-Tibet plateau/Late Pleistocene/pan-lake event/palaeoclimateKey words
Qinghai-Tibet plateau/Late Pleistocene/pan-lake event/palaeoclimate分类
天文与地球科学引用本文复制引用
..Evidence of the Pan-Lake Stage in the Period of 40- 28 ka B.P. on the Qinghai-Tibet Plateau[J].地质学报（英文版）,2000,74(2):266-272,7.基金项目
This research was supported by the National Natural Science Foundation of China grants 49672116 and 49833010. （）
