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• W2034621827 abstract "Research Article| March 01, 2006 Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range, northern India Lewis A. Owen; Lewis A. Owen 1Department of Geology, University of Cincinnati, Cincinnati, Ohio 45221, USA Search for other works by this author on: GSW Google Scholar Marc W. Caffee; Marc W. Caffee 2Department of Physics, Purdue Rare Isotope Measurement (PRIME) Laboratory, Purdue University, West Lafayette, Indiana 47907, USA Search for other works by this author on: GSW Google Scholar Kelly R. Bovard; Kelly R. Bovard 3U.S. Geological Survey, Department of Earth Sciences, University of California, Riverside, California 92521, USA Search for other works by this author on: GSW Google Scholar Robert C. Finkel; Robert C. Finkel 4Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94550, USA Search for other works by this author on: GSW Google Scholar Milap C. Sharma Milap C. Sharma 5Centre for the Study of Regional Development, Jawaharlal Nehru University, New Delhi 110 067, India Search for other works by this author on: GSW Google Scholar Author and Article Information Lewis A. Owen 1Department of Geology, University of Cincinnati, Cincinnati, Ohio 45221, USA Marc W. Caffee 2Department of Physics, Purdue Rare Isotope Measurement (PRIME) Laboratory, Purdue University, West Lafayette, Indiana 47907, USA Kelly R. Bovard 3U.S. Geological Survey, Department of Earth Sciences, University of California, Riverside, California 92521, USA Robert C. Finkel 4Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, California 94550, USA Milap C. Sharma 5Centre for the Study of Regional Development, Jawaharlal Nehru University, New Delhi 110 067, India Publisher: Geological Society of America Received: 29 Oct 2004 Revision Received: 28 May 2005 Accepted: 31 Aug 2005 First Online: 08 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Geological Society of America GSA Bulletin (2006) 118 (3-4): 383–392. https://doi.org/10.1130/B25750.1 Article history Received: 29 Oct 2004 Revision Received: 28 May 2005 Accepted: 31 Aug 2005 First Online: 08 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Lewis A. Owen, Marc W. Caffee, Kelly R. Bovard, Robert C. Finkel, Milap C. Sharma; Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range, northern India. GSA Bulletin 2006;; 118 (3-4): 383–392. doi: https://doi.org/10.1130/B25750.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract Terrestrial cosmogenic nuclide surface exposure dating of moraine boulders and alluvial fan sediments define the timing of five glacial advances over at least the last five glacial cycles in the Ladakh Range of the Transhimalaya. The glacial stages that have been identified are: the Indus Valley glacial stage, dated at older than 430 ka; the Leh glacial stage occurring in the penultimate glacial cycle or older; the Kar glacial stage, occurring during the early part of the last glacial cycle; the Bazgo glacial stage, at its maximum during the middle of the last glacial cycle; and the early Holocene Khalling glacial stage. The exposure ages of the Indus Valley moraines are the oldest observed to date throughout the Himalayan orogen. We observe a pattern of progressively more restricted glaciation during the last five glacial cycles, likely indicating a progressive reduction in the moisture supply necessary to sustain glaciation. A possible explanation is that uplift of Himalayan ranges to the south and/or of the Karakoram Mountains to the west of the region may have effectively blocked moisture supply by the south Asian summer monsoon and mid-latitude westerlies, respectively. Alternatively, this pattern of glaciation may reflect a trend of progressively less extensive glaciation in mountain regions that has been observed globally throughout the Pleistocene. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2034621827 title "Terrestrial cosmogenic nuclide surface exposure dating of the oldest glacial successions in the Himalayan orogen: Ladakh Range, northern India" @default.
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