气候变化领域集成服务门户(CCPortal): Late Cenozoic fluvial-lacustrine susceptibility increases in the Linxia Basin and their implications for Tibetan Plateau uplift

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DOI	10.1016/j.quaint.2013.12.046
	Late Cenozoic fluvial-lacustrine susceptibility increases in the Linxia Basin and their implications for Tibetan Plateau uplift
	Yan, Xiaoli; Miao, Yunfa; Zan, Jinbo; Zhang, Weilin; Wu, Song
通讯作者	Miao, YF (通讯作者)
发表日期	2014
ISSN	1040-6182
EISSN	1873-4553
起始页码	132
结束页码	140
卷号	334
英文摘要	The variations and mechanisms of fluvial-lacustrine mass-specific magnetic susceptibility (x) in the northeastern (NE) Tibetan Plateau are complex. In this study, we compiled two Miocene-Pliocene chi records (the Heilinding and Maogou sections, respectively) from the Linxia Basin fluvial-lacustrine sediments, NE Tibetan Plateau to describe the chi increases and discuss their influential factors. The chi in the Heilinding section remained relatively stable at low values before ca. 8.5 Ma, and has increased since ca. 8.5 Ma with strong fluctuations. In the Maogou section the chi increased at ca. 6.0 Ma with relatively weak fluctuations. The mean chi values were higher in the Heilinding section than the Maogou section. The rock magnetic results showed that hematite dominated both sites during the early periods (>8.5 Ma in the Heilinding and >6.0 Ma in the Maogou, respectively), and was replaced by magnetite after that time. Based on the comparison of chi records in Linxia Basin with other magnetic and climate records from the surrounding regions, the chi increase around 8.5-6.0 Ma in the Linxia Basin was mainly driven by tectonics in the northeastern Tibetan Plateau. (C) 2013 Elsevier Ltd and INQUA. All rights reserved.
关键词	RESOLUTION MAGNETO STRATIGRAPHY CHINESE LOESS LATE MIOCENE TECTONIC UPLIFT ROCK MAGNETISM QAIDAM BASIN QINGHAI PROVINCE EOLIAN SEDIMENTS CARBON-CYCLE GUIDE BASIN
语种	英语
WOS研究方向	Physical Geography ; Geology
WOS类目	Geography, Physical ; Geosciences, Multidisciplinary
WOS记录号	WOS:000338817800014
来源期刊	QUATERNARY INTERNATIONAL
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/258298
推荐引用方式 GB/T 7714	Yan, Xiaoli,Miao, Yunfa,Zan, Jinbo,et al. Late Cenozoic fluvial-lacustrine susceptibility increases in the Linxia Basin and their implications for Tibetan Plateau uplift[J]. 中国科学院青藏高原研究所,2014,334.
APA	Yan, Xiaoli,Miao, Yunfa,Zan, Jinbo,Zhang, Weilin,&Wu, Song.(2014).Late Cenozoic fluvial-lacustrine susceptibility increases in the Linxia Basin and their implications for Tibetan Plateau uplift.QUATERNARY INTERNATIONAL,334.
MLA	Yan, Xiaoli,et al."Late Cenozoic fluvial-lacustrine susceptibility increases in the Linxia Basin and their implications for Tibetan Plateau uplift".QUATERNARY INTERNATIONAL 334(2014).