ISL OpenIR  > 青海盐湖研究所知识仓储
青海湖的形成与演化趋势
袁宝印; 陈克造; J.M.Bowler; 叶素娟
1990-10-01
Source Publication第四纪研究
Issue3Pages:233-243
Abstract青海湖盆地形成于上新世,湖泊至晚在0.5 Ma前已经形成,在初期有流向贵德盆地的出口。湖泊发育主要划分为三个阶段:中更新世湖泊最盛期、晚更新世湖泊稳定期和全新世湖泊收缩期。晚更新世早期由于湖泊强烈沉陷,使河流出口处相对抬高,河水倒流而形成倒淌河。第四纪以来,我国西北地区有气候逐渐变干的趋势,导致全新世以来青海湖不断收缩。如不采取人工措施,青海湖还将继续收缩。
Keyword古湖岸线 湖积台地 湖蚀陡崖 湖泊演化
Language中文
Document Type期刊论文
Identifierhttp://ir.isl.ac.cn/handle/363002/1466
Collection青海盐湖研究所知识仓储
Recommended Citation
GB/T 7714
袁宝印,陈克造,J.M.Bowler,等. 青海湖的形成与演化趋势[J]. 第四纪研究,1990(3):233-243.
APA 袁宝印,陈克造,J.M.Bowler,&叶素娟.(1990).青海湖的形成与演化趋势.第四纪研究(3),233-243.
MLA 袁宝印,et al."青海湖的形成与演化趋势".第四纪研究 .3(1990):233-243.
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