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DOI	10.1130/G38583.1
	Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon
	Ding, Lin; Spicer, R. A.; Yang, Jian; Xu, Qiang; Cai, Fulong; Li, Shun; Lai, Qingzhou; Wang, Houqi; Spicer, T. E. V.; Yue, Yahui; Shukla, A.; Srivastava, G.; Khan, M. Ali; Bera, S.; Mehrotra, R.
通讯作者	Ding, L (通讯作者)
发表日期	2017
ISSN	0091-7613
EISSN	1943-2682
起始页码	215
结束页码	218
卷号	45 期号:3
英文摘要	We reconstruct the rise of a segment of the southern flank of the Himalaya-Tibet orogen, to the south of the Lhasa terrane, using a paleoaltimeter based on paleoenthalpy encoded in fossil leaves from two new assemblages in southern Tibet (Liuqu and Qiabulin) and four previously known floras from the Himalaya foreland basin. U-Pb dating of zircons constrains the Liuqu flora to the latest Paleocene (ca. 56 Ma) and the Qiabulin flora to the earliest Miocene (21- 19 Ma). The proto-Himalaya grew slowly against a high (similar to 4 km) proto-Tibetan Plateau from similar to 1 km in the late Paleocene to similar to 2.3 km at the beginning of the Miocene, and achieved at least similar to 5.5 km by ca. 15 Ma. Contrasting precipitation patterns between the Himalaya-Tibet edifice and the Himalaya foreland basin for the past similar to 56 m.y. show progressive drying across southern Tibet, seemingly linked to the uplift of the Himalaya orogen.
关键词	HYDROTHERMAL DOLOMITE SUEZ RIFT
语种	英语
WOS研究方向	Geology
WOS类目	Geology
WOS记录号	WOS:000396125100006
来源期刊	GEOLOGY
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/259069
推荐引用方式 GB/T 7714	Ding, Lin,Spicer, R. A.,Yang, Jian,et al. Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon[J]. 中国科学院青藏高原研究所,2017,45(3).
APA	Ding, Lin.,Spicer, R. A..,Yang, Jian.,Xu, Qiang.,Cai, Fulong.,...&Mehrotra, R..(2017).Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon.GEOLOGY,45(3).
MLA	Ding, Lin,et al."Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon".GEOLOGY 45.3(2017).