汾河地堑湖盆第四纪地貌—沉积特征的构造控制

doi:10.11821/xb201001008

Abstract

Abstract:

The field work found that there existed three abrupt lake regressions in the Fenhe River Graben Basins during the middle-late Quaternary,which were consistent with the development of paleosols S₈,S₅ and S₁.This indicates that those regressions are not the results of the dry climate but due to the neotectonic movement.The basins experienced slow transgressions when the loess-paleosols between S₁₁-S₈,S₈-S₅ and S₅-S₁ developed,and sank after S₁ had formed.Based on these discoveries and previously revealed data about the activities of the upper mantle in the deep earth around this region,the paper puts forward a hypothesis that can explain how the lake transgression-regression cycles took place under the control of the neotectonic movement.The morpho-sedimentary characteristics are the results and responses of the activities of the upper mantle in the deep earth.

Key words: Fenhe River, Quaternary, lake landform, lacustrine sedimentation, lake transgression and regression

CLC Number:

P931

HU Xiaomeng; GUO Jiaxiu; HU Xiangyang. The Development of Morpho-sediment of Quaternary in Fenhe River Graben Basins and the Neotectonic Movement[J].Acta Geographica Sinica, 2010, 65(1): 73-81.

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The Development of Morpho-sediment of Quaternary in Fenhe River Graben Basins and the Neotectonic Movement

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