摘要
根据 2 6 0 3a有史记载以来黄河河道变迁和春秋以来东平湖演变历史 ,本文提出我国中央山系东段碰撞和松弛导致的地势上升和下降是影响黄河河道变迁和东平湖演变的重要因素。山系碰撞上升造成黄河河道向北西迁移 ,东平湖湿地北漫 ;山系松弛下降导致黄河河道向东南迁移 ,东平湖南泛。
According to the shifting of Yellow River from the historic recorder of 2603 years and the evolutionary history of Dongping Lake, this paper proposes that the elevation and decline caused by collision and relexation of the eastern sector of the central mountain system in our country are the important factors influencing on the shifting of Yellow River and the evolution of Dongping Lake. Collision and elevation made the channel of Yellow River shift to the northewst and Dongping Lake flood northwards, while relexation and decline led the channel of Yellow River shift to the southeast and Dongping Lake flood southwards.
出处
《山东农业大学学报（自然科学版）》
CSCD
北大核心
2004年第3期391-394,共4页
Journal of Shandong Agricultural University：Natural Science Edition
关键词
河道
黄河
东平湖
记载
下降
湿地
中央
中国
重要因素
影响
central mountain system, Tancheng-Lujiang fault, Yellow River,Dongping Lake,Dongpinghu wetland
