Taihu Lake evolution 太湖演变
Modern Dongting Lake evolution 近代洞庭湖演变
lake evolution and environmental change 湖泊演化与环境变化
lake basin evolution 湖盆演化
evolution of lake 湖沼演变
Huadian Basin is a small-scale half-graben basin,and F1 fault in the southern margin of the basin controls the Palaogene lake evolution.
桦甸盆地为小型半地堑盆地,盆地南缘F1断裂控制了古近系湖泊演化特征。
参考来源 - 古湖泊学研究——以桦甸断陷盆地为例·2,447,543篇论文数据，部分数据来源于NoteExpress
The new data have been provided for the lake evolution, the climate change, the paleogeographic changes and the divide Quaternary period.
为研究该区湖泊演化、气候变化、古地理变迁及第四系划分等提供了新资料。
According to the measured data of typical inland lakes in northwest China, this research has revealed the characteristics of lake evolution and their mechanism during the past 40 years.
利用40年来的实测数据研究揭示了西北典型内陆湖泊的演化特点及机制。
The evolution of Lake Dongting is determined by three main factors, which are tectonic subsidence, siltation and human impacts.
洞庭湖的演变主要受构造沉降、泥沙淤积和人类活动影响三大因素的控制。
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