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《Acta Geographica Sinica》 2002-03
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Response of Landform Development to the Tectonic Movement and the Climate Changes in Fenhe Drainage Basin

HU Xiaomeng, FU Jianli2, LI Youli2l. The Urdan and Tourism Schoo1, Shanghai Normal University Shanghai 200234, China;2. Department of Urban and Environmenta1 Science, Peking University Beijing l00871, China  
Based on analysis of the characteristics of the terraces in patterns and sediment ofthe Fenhe drainage basin, we find it was the three tectonic uplifts that caused the formation ofthree-level terraces. These uplifts took place at 0.76 Ma BP, 0.55 Ma BP and 0.l3 Ma BPrespectively and resulted in the three low-level stages of the paleolake in consistent with thedevelopment of S8, S5, S1, in time. Compared with the neotectonic movements in the upperreaches of the Yellow River, the three tectonic uplifts in this region are in correspondence withthem, and this may imply that the neotectonic uplifts of the Qinghai-Tibet Plateau strongycontrolled the tectonic movements in the Fenhe drainage basin. According to the features oflaustrine sediment deposited from the time when S5, ended its formation to the time when S1,began to develop, we also find the changes in paleoclimate from dry to wet influenced thedevelopment of the paleolakes. The lake levels rose when it was wet and dropped when it wasdry, but the extent of this change of the lake levels was no more than 4.5 m, and much smallerthan that caused by tectonic moveme.
【Fund】: 国家自然科学基金资助项目(40071016)
【CateGory Index】: P931
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