Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China: Implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene

doi:10.1016/j.geomorph.2016.03.034

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	Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China: Implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene
	Jia, Liyun 1; Zhang, Xujiao 2; Ye, Peisheng 1; Zhao, Xitao 3; He, Zexin 2; He, Xiangli 2; Zhou, Qingshuo 2; Li, Jie 2; Ye, Mengni 2; Wang, Zhen 2
刊名	GEOMORPHOLOGY
	2016-06-15
卷号	263 页码:87-98
关键词	Hetao Basin Yellow River River terrace Paleolake Dating Terrace sediments
DOI	10.1016/j.geomorph.2016.03.034
文献子类	Article
英文摘要	Terrace formation processes can reflect the evolution of large rivers. The Hetao Basin is a floodplain of the Yellow River, and there are two to three terraces that extend E-W on the northern margin. Based on a detailed field geological survey and measurement of the terrace sections, combined with sedimentological and chronological analyses, we reconstructed the developmental processes of the three terraces and inferred that three river terraces were formed by the Yellow River. The OSL dating results show that the time of deposition of terrace 3 was prior to 118 ka BP. Subsequently, the terrace began to experience incision and formed the geomorphic surface of terrace T3. Similarly, terrace 2 and terrace 1 were mainly deposited from similar to 109 and 59 ka, respectively; and began to be incised prior to 71 and 46 ka, respectively. The three terraces in the northern Hetao Basin are the products of the combined actions of climatic shifts and tectonic uplift. The Yellow River's evolutionary history in the Hetao area since the Late Pleistocene is discussed. Before about 120 ka BP, the Yellow River may have flowed through the northern Hetao Basin. Between 110 and 70 ka BP, the Yellow River experienced at least two changes between river and lake sedimentation. From 60 to 50 ka, a very large river-connected lake of the Yellow River was developed in the Hetao Basin. After 50 ka, the Hetao river-connected paleolake of the Yellow River gradually dried. (C) 2016 Elsevier B.V. All rights reserved.
WOS关键词	REGENERATIVE-DOSE PROTOCOL ; BETIC CORDILLERA ; LATE QUATERNARY ; UPLIFT-DRIVEN ; ORDOS PLATEAU ; CLIMATE ; SYSTEMS ; LUMINESCENCE ; SEQUENCES ; INCISION
WOS研究方向	Physical Geography ; Geology
语种	英语
WOS记录号	WOS:000376712900006
资助机构	1:50,000 pilot mapping of Hulesitaisumu(K48E017024) ; 1:50,000 pilot mapping of Hulesitaisumu(K48E017024) ; Taerhuzhen(K48E018024) ; Taerhuzhen(K48E018024) ; Fuxingcheng(K48E019024) ; Fuxingcheng(K48E019024) ; Jiergalangtuxiang(K48E020024 ; Jiergalangtuxiang(K48E020024 ; palaeoclimate evolutional variations and genetic mechanisms in various monsoon regions of China(201211077) ; palaeoclimate evolutional variations and genetic mechanisms in various monsoon regions of China(201211077) ; 12120114042101) ; 12120114042101) ; 1:50,000 pilot mapping of Hulesitaisumu(K48E017024) ; 1:50,000 pilot mapping of Hulesitaisumu(K48E017024) ; Taerhuzhen(K48E018024) ; Taerhuzhen(K48E018024) ; Fuxingcheng(K48E019024) ; Fuxingcheng(K48E019024) ; Jiergalangtuxiang(K48E020024 ; Jiergalangtuxiang(K48E020024 ; palaeoclimate evolutional variations and genetic mechanisms in various monsoon regions of China(201211077) ; palaeoclimate evolutional variations and genetic mechanisms in various monsoon regions of China(201211077) ; 12120114042101) ; 12120114042101)
内容类型	期刊论文
源URL	[http://ir.iggcas.ac.cn/handle/132A11/53435]
专题	地质与地球物理研究所_其他部门
作者单位	1.Chinese Acad Geol Sci, Inst Geomech, Beijing 100081, Peoples R China 2.China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China 3.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China
推荐引用方式 GB/T 7714	Jia, Liyun,Zhang, Xujiao,Ye, Peisheng,et al. Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China: Implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene[J]. GEOMORPHOLOGY,2016,263:87-98.
APA	Jia, Liyun.,Zhang, Xujiao.,Ye, Peisheng.,Zhao, Xitao.,He, Zexin.,...&Meng, Jing.(2016).Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China: Implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene.GEOMORPHOLOGY,263,87-98.
MLA	Jia, Liyun,et al."Development of the alluvial and lacustrine terraces on the northern margin of the Hetao Basin, Inner Mongolia, China: Implications for the evolution of the Yellow River in the Hetao area since the late Pleistocene".GEOMORPHOLOGY 263(2016):87-98.