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
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。
The new data have been provided for the lake evolution, the climate change, the paleogeographic changes and the divide Quaternary period.
为青藏高原湖泊演化、气候环境变迁研究及第四纪地层的划分与对比提供了新资料。
These supply a new information for the evolution of the Qinghai-Tibet Plateau lakes, climate change research and the division and correlation of the Quaternary strata.
宁晋泊沉积物的环境指标高分辨率分析，揭示了全新世温暖期以来气候变化规律和湖泊演化过程。
Climatic fluctuation and process of lake changes were revealed through high resolution analysis on environmental indices based on sediments of Ningjin lake.
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