The Spatial and Temporal Features of Surface Uplift in Loess Plateau since 0.8 Ma

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The Spatial and Temporal Features of Surface Uplift in Loess Plateau since 0.8 Ma

详细信息

责任者：Hu Chunsheng (Department of Geography ; Anhui Normal University ; Wuhu 241000 ; China) ; Pan Baotian
刊名：Scientia Geographica Sinica
出版年：2012
卷期：31(9)
关键词：隆起 ; uplifts ; 黄土高原 ; Loess Plateau
页码：p.1131-1135
图表：illus., 3 tbales, 27 refs.
分类号：0300
issnNo：ISSN1000-0690
isbnNo：CN22-1124/P

摘要

PAN style="DISPLAY: inline! important; FLOAT: none; WORD-SPACING: 0px; FONT: 12px/22px Arial, 宋体; TEXT-TRANSFORM: none; COLOR: rgb(36,36,36); TEXT-INDENT: -5px; WHITE-SPACE: normal; LETTER-SPACING: normal; BACKGROUND-COLOR: rgb(244,244,244); TEXT-ALIGN: left; WIDOWS: 2; ORPHANS: 2; -webkit-text-size-adjust: auto; -webkit-text-stroke-width: 0px">By analyzing the characteristics of the Yellow River terraces in Loess Plateau,it is presented that the terraces are mainly tectonic genesis,and formed after the Yellow River reached a quasi-equilibrium state.According to the research on the Yellow River terraces at 0.8 Ma in the Loess Plateau and the correlative literature,this paper verifies that there was a large-scale surface uplift at about 0.8 Ma in the Loess Plateau,and the surface uplift resulted in river incision and terrace formation.The paper also proposes that the surface uplift of the Loess Plateau since 0.8 Ma is related to the surface uplift of the Qinghai-Tibetan Plateau.

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