Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/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
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ISSN | 0277-3791 |
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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