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| 喜马拉雅山佩枯岗日冰川地貌的年代学、平衡线高度和气候研究 | |
| 引用本文： | 刘耕年,Li Yingkui,陈艺鑫,张梅,李川川,孔屏,Harbor J.,Caffee M.W..喜马拉雅山佩枯岗日冰川地貌的年代学、平衡线高度和气候研究[J].冰川冻土,2011,33(5):959-970. |
| 作者姓名： | 刘耕年 Li Yingkui 陈艺鑫 张梅 李川川 孔屏 Harbor J. Caffee M.W. |
| 作者单位： | 1. 北京大学城市与环境学院,北京,100871 2. Department of Geography, University of Tennessee, Knoxville, TN 37996, USA 3. 中国科学院地质与地球物理研究所,北京,100029 4. Department of Earth and Atmospheric Sciences, Purdue University, West Lafayette, IN 47907, USA 5. Department of Physics/PRIME Laboratory, Purdue University, West Lafayette, IN 47907, USA |
| 基金项目： | 国家自然科学基金项目(40571014;40971002); University of Missouri Research Board(UB-07-042)资助 |
| 摘 要： | 喜马拉雅山珠穆朗玛峰-希夏邦马峰地区是青藏高原南部现代冰川集中发育区之一,古冰川遗迹亦十分丰富,是研究第四纪青藏高原冰川形成和演化的关键区,一直备受地貌和第四纪环境研究者的关注.应用原地宇宙核素10Be暴露年龄测试技术,对采自希夏邦马峰西北佩枯岗日拉曲谷地冰碛垄上的冰川漂砾进行年代学研究;结合冰川地貌分析方法,对古冰川... |
| 关 键 词： | 喜马拉雅山 冰川地貌 宇宙核素 年代学 气候 |
Glacial Landform Chronology and Environment Reconstruction of Peiku Gangri,Himalayas |
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| LIU Geng-nian,LI Ying-kui,CHEN Yi-xin,ZHANG Mei,LI Chuan-chuan,KONG Ping,Harbor J.,Caffee M.W..Glacial Landform Chronology and Environment Reconstruction of Peiku Gangri,Himalayas[J].Journal of Glaciology and Geocryology,2011,33(5):959-970. | |
| Authors: | LIU Geng-nian LI Ying-kui CHEN Yi-xin ZHANG Mei LI Chuan-chuan KONG Ping Harbor J Caffee MW |
| Institution: | LIU Geng-nian1,LI Ying-kui2,CHEN Yi-xin1,ZHANG Mei1,LI Chuan-chuan,KONG Ping3,Harbor J.4,Caffee M.W.5(1.College of Urban and Environmental Sciences,Peking University,Beijing 100871,China,2.Department of Geography,University of Tennessee,Knoxville,TN 37996,USA,3.Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029,4.Department of Earth and Atmospheric Sciences,Purdue University,West Lafayette,IN 47907,5.Department of Physics/PRIME Laboratory,West Lafay... |
| Abstract: | Xixabangma-Qomolangma(Xixabangma-Everest) region is an intensively glaciation centre in monsoonal Himalayas,and relic glacial landforms are widely distributed in the glacial valley.Relatively well preserved geomorphic and sedimentary sequences make the region to be a key region for reconstructing Quaternary glaciations and environmental evolution in the Tibetan Plateau.Based on field geomorphologic surveying and 10Be terrestrial cosmogenic nuclide(TCN) exposure dating,Quaternary glacial events in the Laqu v... |
| Keywords: | Himalayas glacial landform TCN dating climate |
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