Arid
DOI10.1016/j.quascirev.2013.07.025
Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen
Dortch, Jason M.1; Owen, Lewis A.2; Caffee, Marc W.3
通讯作者Dortch, Jason M.
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
出版年2013
卷号78页码:188-208
英文摘要

Mapping and forty-seven new Be-10 ages help define the timing of glaciation in the Ladakh and Pangong Ranges in Northwest India. Five new local glacial stages are defined for the Ladakh Range. From oldest to youngest these include: the Ladakh-4 glacial stage at 81 +/- 20 ka; the Ladakh-3 glacial stage (not dated); the Ladakh-2 glacial stage at 22 +/- 3 ka; the Ladakh-1 glacial stage (not dated); and the Ladakh Cirque glacial stage at 1.8 +/- 0.4 ka. Three local glacial stages are defined for the Pangong Range, which include: the Pangong-2 glacial stage at 85 +/- 15 ka; the Pangong-1 glacial stage at 40 +/- 3 ka; and the Pangong Cirque glacial stage at 0.4 +/- 0.3 ka. The new Be-10 ages are combined with 645 recalculated Be-10 ages from previous studies to develop the first regional framework of glaciation across the dryland regions of the Greater Himalaya, Transhimalaya, Pamir and Tian Shan at the western end of the Himalayan-Tibetan orogen. Nineteen regional glacial stages are recognized that are termed semi-arid western Himalayan-Tibetan stages (SWHTS). These include: SWHTS 9 at 311 +/- 32 ka; SWHTS 7 at 234 +/- 44 ka [tentative]; SWHTS 6 at 146 +/- 18 ka; SWHTS 5E at 121 +/- 11 ka; SWHTS 5A at 80 +/- 5 ka; SWHTS 5A- at 72 +/- 8 ka; SWHTS 4 at 61 +/- 5 ka; SWHTS 3 at 46 +/- 4 ka; SWHTS 2F at 30 +/- 3 ka; SWHTS 2E at 20 +/- 2 ka; SWHTS 20 at 16.9 +/- 0.7 ka; SWHTS 2C at 14.9 +/- 0.8 ka; SWHTS 2B at 13.9 +/- 0.5 ka; SWHTS 2A at 12.2 +/- 0.8 ka; SWHTS 1E at 8.8 +/- 0.3 ka [tentative]; SVVHTS 1D at 6.9 +/- 0.2 ka [tentative]; SWHTS 1C at 3.8 +/- 0.6 ka; SWHTS 1B at 1.7 +/- 0.2 ka; and SWHTS 1A at 0.4 +/- 0.1 ka. Regional glacial stages older than 21 ka are broadly correlated with strong monsoons. SWHTS that are 21 ka or younger, have smaller uncertainties and broadly correlate with global ice volume given by marine Oxygen Isotope Stages, and northern hemisphere climatic events (Oldest Dryas, Older Diyas, Younger Dryas, Roman Humid Period, and Little Ice Age). Crown Copyright (C) 2013 Published by Elsevier Ltd. All rights reserved.


英文关键词Cosmogenic radionuclide dating Himalaya Tibet Glaciation Moraine Chronology Gaussian
类型Article
语种英语
国家England ; USA
收录类别SCI-E
WOS记录号WOS:000327908900013
WOS关键词LATE QUATERNARY GLACIATION ; BE-10 PRODUCTION-RATES ; SURFACE EXPOSURE AGES ; LADAKH BATHOLITH ; PLEISTOCENE GLACIATIONS ; NORTHWESTERN HIMALAYA ; LANDSCAPE EVOLUTION ; KARAKORAM FAULT ; NORTHERN INDIA ; MUZTAG ATA
WOS类目Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向Physical Geography ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/179644
作者单位1.Univ Manchester, Sch Environm & Dev, Manchester M0 1QD, Lancs, England;
2.Univ Cincinnati, Dept Geol, Cincinnati, OH 45221 USA;
3.Purdue Univ, Dept Phys, PRIME Lab, W Lafayette, IN 47906 USA
推荐引用方式
GB/T 7714
Dortch, Jason M.,Owen, Lewis A.,Caffee, Marc W.. Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen[J],2013,78:188-208.
APA Dortch, Jason M.,Owen, Lewis A.,&Caffee, Marc W..(2013).Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen.QUATERNARY SCIENCE REVIEWS,78,188-208.
MLA Dortch, Jason M.,et al."Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen".QUATERNARY SCIENCE REVIEWS 78(2013):188-208.
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