Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma

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	Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma
	Zhang, ZK; Wang, SM; Yang, XD; Jiang, FH; Shen, J; Li, XS
刊名	QUATERNARY INTERNATIONAL
	2004
卷号	117 期号:0 页码:35-40
ISSN号	1040-6182
英文摘要	Yellow River erosion through Longyang Gorge and Sanmen Gorge at 0.15 Ma corresponds with a rapid uplifting of the Qinghai-Xizang (Tibet) Plateau and strong incision in the middle and upper reaches of the Yellow River. Evidence from the upper reaches, middle reaches and lower reaches suggests that this event was controlled by intensive tectonic movement and climatic change. Evidence suggests that the onset of the last interglacial in the upper reaches began a little earlier than 0.15 Ma, and coincides with lake sedimentary records, and oxygen isotope records from the Guliya ice core in the Tibet Plateau. (C) 2003 Elsevier Ltd and INQUA. All rights reserved.
公开日期	2012-03-06
内容类型	期刊论文
源URL	[http://159.226.73.51/handle/332005/2751]
专题	南京地理与湖泊研究所_湖泊室
推荐引用方式 GB/T 7714	Zhang, ZK,Wang, SM,Yang, XD,et al. Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma[J]. QUATERNARY INTERNATIONAL,2004,117(0):35-40.
APA	Zhang, ZK,Wang, SM,Yang, XD,Jiang, FH,Shen, J,&Li, XS.(2004).Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma.QUATERNARY INTERNATIONAL,117(0),35-40.
MLA	Zhang, ZK,et al."Evidence of a geological event and environmental change in the catchment area of the Yellow River at 0.15 Ma".QUATERNARY INTERNATIONAL 117.0(2004):35-40.