气候变化领域集成服务门户(CCPortal): High-resolution magneto stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau

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DOI	10.1016/j.epsl.2007.03.042
	High-resolution magneto stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau
	Fang, Xiaomin; Zhang, Weilin; Meng, Qingquan; Gao, Junping; Wang, Xiaoming; King, John; Song, Chunhui; Dai, Shuang; Miao, Yunfa
发表日期	2007
ISSN	0012-821X
EISSN	1385-013X
起始页码	293
结束页码	306
卷号	258 期号:1-2
英文摘要	The closed inland Qaidam Basin in the NE Tibetan Plateau contains possibly the world's thickest (similar to 12,000 in) continuous sequence of Cenozoic fluviolacustrine sedimentary rocks. This sequence contains considerable information on the history of Tibetan uplift and associated climatic change. However, work within Qaidam Basin has been held back by a paucity of precise time constraints on this sequence. Here we report on a detailed paleomagnetic study of the well exposed 4570 m Huaitoutala section along the Keluke anticline in the northeastern Qaidam Basin, where three distinct faunas were recovered and identified from the middle Miocene through Pliocene. Constrained by these faunal ages, the observed thirty-three pairs of normal and reversed polarity zones can be readily correlated with chrons 2n-5Br of the GPTS. This study assigns the age of the section to the interval between ca. 15.7 Ma to 1.8 Ma. In addition, the widely used stratigraphic units the Xia Youshashan, Shang Youshashan, the Shizigou and Qigequan Fort-nations were formed at >15.3 Ma, 15.3-8.1 Ma, 8.1-2.5 Ma and <2.5 Ma, respectively. We obtained a very high average sedimentation rate of similar to 33 cm/ka over the entire interval 15.7 to 1.8 Ma. Furthermore, the average sedimentation rate is punctuated by three intervals of persistent rapid increases starting at about similar to 14.7 Ma, 8.1 Ma and 3.6 Ma. These intervals are interpreted as times of rapid uplift and fast exhumation of the NE Tibetan Plateau. (C) 2007 Published by Elsevier B.V.
关键词	ALTYN-TAGH FAULT CENOZOIC TECTONICS TERTIARY DEPOSITS FISSION-TRACK GUIDE BASIN TIAN-SHAN MAGNETOSTRATIGRAPHY MARGIN DISPLACEMENT MAGNITUDE
英文关键词	magnetostratigraphy; Neogene; Qaidam Basin; NE Tibetan Plateau
语种	英语
WOS研究方向	Geochemistry & Geophysics
WOS类目	Geochemistry & Geophysics
WOS记录号	WOS:000247828000023
来源期刊	EARTH AND PLANETARY SCIENCE LETTERS
来源机构	中国科学院青藏高原研究所
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/257511
推荐引用方式 GB/T 7714	Fang, Xiaomin,Zhang, Weilin,Meng, Qingquan,et al. High-resolution magneto stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau[J]. 中国科学院青藏高原研究所,2007,258(1-2).
APA	Fang, Xiaomin.,Zhang, Weilin.,Meng, Qingquan.,Gao, Junping.,Wang, Xiaoming.,...&Miao, Yunfa.(2007).High-resolution magneto stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau.EARTH AND PLANETARY SCIENCE LETTERS,258(1-2).
MLA	Fang, Xiaomin,et al."High-resolution magneto stratigraphy of the Neogene Huaitoutala section in the eastern Qaidam Basin on the NE Tibetan Plateau, Qinghai Province, China and its implication on tectonic uplift of the NE Tibetan Plateau".EARTH AND PLANETARY SCIENCE LETTERS 258.1-2(2007).