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Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon
Ding, Lin1; Spicer, R. A.; Yang, Jian; Xu, Qiang1; Cai, Fulong1; Li, Shun1; Lai, Qingzhou1; Wang, Houqi1; Spicer, T. E. V.; Yue, Yahui1; Shukla, A.; Srivastava, G.; Khan, M. Ali; Bera, S.; Mehrotra, R.
2017
发表期刊GEOLOGY
ISSN0091-7613
卷号45期号:3页码:215-218
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.
学科领域Forestry ; Physical Geography
DOI10.1016/j.dendro.2016.01.005
收录类别SCI
语种英语
WOS关键词HYDROTHERMAL DOLOMITE ; SUEZ RIFT
WOS记录号WOS:000406004600002
出版者GEOLOGICAL SOC AMER, INC
文献子类Article
出版地BOULDER
EISSN1943-2682
资助机构Industry Technology Facilitator project PSD by BG-Group [3310PSD] ; Saudi Aramco ; Statoil ; TotalTotal SA ; Natural Environment Research Council (NERC) Facility award at the NERC Isotope Community Support Facility at SUERC [IP-1357-1112]
作者邮箱dinglin@itpcas.ac.cn ; r.a.spicer@open.ac.uk ; yangjian@ibcas.ac.cn
引用统计
被引频次:8[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.ibcas.ac.cn/handle/2S10CLM1/22078
专题系统与进化植物学国家重点实验室
作者单位1.Chinese Acad Sci, Inst Tibetan Plateau Res, Key Lab Continental Collis & Plateau Uplift, Beijing 100101, Peoples R China
2.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China
3.Spicer, R. A.; Yang, Jian; Spicer, T. E. V.] Chinese Acad Sci, Inst Bot, State Key Lab Systemat & Evolutionary Bot, Beijing 100093, Peoples R China
4.Spicer, R. A.] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England
5.Shukla, A.; Srivastava, G.; Mehrotra, R.] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India
6.Khan, M. Ali; Bera, S.] Univ Calcutta, Dept Bot, Ctr Adv Study, Kolkata 700019, India
7.Bera, S.] Sidho Kanho Birsha Univ, Dept Bot, Ranchi Rd, Purulia 723104, India
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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]. GEOLOGY,2017,45(3):215-218.
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),215-218.
MLA Ding, Lin,et al."Quantifying the rise of the Himalaya orogen and implications for the South Asian monsoon".GEOLOGY 45.3(2017):215-218.
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