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临汾凹陷晚更新世以来河流阶地堆积的构造响应
引用本文:马志正,范晋芳,马新红,张亚群,胡小猛,钱秀杰. 临汾凹陷晚更新世以来河流阶地堆积的构造响应[J]. 山西师范大学学报:自然科学版, 2010, 0(4)
作者姓名:马志正  范晋芳  马新红  张亚群  胡小猛  钱秀杰
作者单位:山西师范大学城市与环境科学学院;临汾职业技术学院;临汾市尧都区地震局;山西省晋中市榆次一中;上海师范大学地理与旅游学院;云南省大理市三中;
基金项目:国家自然科学基金(40671018)
摘    要:河流阶地是地表侵蚀与堆积过程中出现的最普通的地貌形态.但仔细分析,在不同地域、不同历史时段,因构造、地形起伏的程度和气候变迁的影响,沉积物变化很大.本文根据这一特点,研究了临汾凹陷中阶地堆积与构造运动的关系,初步确定了堆积物普遍反映的构造变化特征.

关 键 词:临汾凹陷  河流阶地  堆积物  构造  

Construction Response of River Terraces from Late Pleistocene in Linfen Concavity
MA Zhi-zheng,FAN Jin-fang,MA Xin-hong,ZHANG Ya-qun,HU Xiao-meng,QIAN Xiu-jie. Construction Response of River Terraces from Late Pleistocene in Linfen Concavity[J]. Journal of Shanxi Teachers University, 2010, 0(4)
Authors:MA Zhi-zheng  FAN Jin-fang  MA Xin-hong  ZHANG Ya-qun  HU Xiao-meng  QIAN Xiu-jie
Affiliation:MA Zhi-zheng1,FAN Jin-fang2,MA Xin-hong3,ZHANG Ya-qun4,HU Xiao-meng5,QIAN Xiu-jie6(1.School of Urban and Environment Science,Shanxi Normal University,Linfen 041004,Shanxi,China,2.Linfen Vocational & Technical College,Linfen 041000,3.Earth Bureau,Yaodu Distict,4.No.1 Middle School of Yuci,Jinzhong 030600,5.School of Environment and Tourism,Shanghai Normal University,Shanghai 200234,6.No.3 Middle School of Dali,Dali 071000,Yunnan,China)
Abstract:River terraces are the most common physiognomy form appearing in the course of terrstrial erosion and accumulation.It varies largely in different areas and historical periods because of the effects on the level of construction and climate.According to the feature,we study the relationship between accumulation terraces and construction movement,then defines the feature of construction changes responded by accumulations.
Keywords:Linfen Concavity  river terrace  accumulation  construction  
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