The Late Cenozoic uplift of the Liupan Shan, China

doi:10.1007/BF02911985

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（1985-2004）

	The Late Cenozoic uplift of the Liupan Shan, China
	Song, YG; Fang, XM; Li, JJ; An, ZS; Miao, XD
	2001-10
发表期刊	SCIENCE IN CHINA SERIES D-EARTH SCIENCES
卷号	44 页码:176-184
文章类型	Article
摘要	Based on paleomagnetic measurements and morphostratigraphy of red bed/clay sequences from pediments of the Liupan Shan and the Longdong Basin, the following results are revealed. The red bed/clay sediments became to accumulate at around 8.1 MaBP, which implied that the plantation surface developed since Late Cretaceous was broken by active fault, and its development was terminated. The Liupan Shan began to slightly uplift. The Liupan Shan experienced a small-scale uplift around 5.2 MaBP, inferred from the appearance of fine gravel sediments at that time. Consequently, a pediment was developed. The Liupan Shan accelerated uplift since about 3.8 MaBP at a large scale, which caused the deep incision of the rivers and the termination of fluvial and lacustrine deposition. Meanwhile, typical eolian red clay appeared since then. This uplift process is well correlated and in response to that of the Tibetan Plateau and the mountains around it.
关键词	magnetostratigraphy red clay/bed tectonic evolution Liupan Shan Late Cenozoic
学科领域	Geology
DOI	10.1007/BF02911985
关键词[WOS]	MAGNETOSTRATIGRAPHY ; TIBET
收录类别	SCI ; SCIE
语种	英语
WOS研究方向	Geosciences, Multidisciplinary
WOS记录号	WOS:000175181800021
出版者	SCIENCE CHINA PRESS
引用统计	被引频次：92[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/11910
专题	黄土与第四纪地质国家重点实验室（1985-2004）
推荐引用方式 GB/T 7714	Song, YG,Fang, XM,Li, JJ,et al. The Late Cenozoic uplift of the Liupan Shan, China[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2001,44:176-184.
APA	Song, YG,Fang, XM,Li, JJ,An, ZS,&Miao, XD.(2001).The Late Cenozoic uplift of the Liupan Shan, China.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,44,176-184.
MLA	Song, YG,et al."The Late Cenozoic uplift of the Liupan Shan, China".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 44(2001):176-184.