[1] |
HANSON M A, LIAN O B, CIAGUE J J. The sequence and timing of large Late Pleistocene floods from glacial Lake Missoula[J]. Quaternary Science Reviews, 2012, 31(1): 67-81.
DOI
URL
|
[2] |
WAITT R B. Case for periodic, colossal jökulhlaups from Pleistocene glacial Lake Missoula[J]. Geological Society of America Bulletin, 1985, 96(10):1271-1286.
DOI
URL
|
[3] |
JIANG H C, MAO X, XU H Y, et al. Provenance and earthquake signature of the last deglacial Xinmocun lacustrine sediments at Diexi, East Tibet[J]. Geomorphology, 2014, 204(1):518-531.
DOI
URL
|
[4] |
WANG P, ZHANG B, QIU W L, et al. Soft-sediment deformation structures from the Diexi paleo-dammed lakes in the upper reaches of the Minjiang River, east Tibet[J]. Journal of Asian Earth Sciences, 2011, 40(4):865-872.
DOI
URL
|
[5] |
ZHANG Y S, ZHAO X T, LAN H X, et al. A Pleistocene landslide-dammed lake, Jinsha River, Yunnan, China[J]. Quaternary International, 2011, 233(1):72-80.
DOI
URL
|
[6] |
RICHARDSON S D, REYNOLDS J M. An overview of glacial hazards in the Himalayas[J]. Quaternary International, 2000, 65/66: 31-47.
DOI
URL
|
[7] |
MONTGOMERY D R, HALLET B, LIU Y P, et al. Evidence for Holocene megafloods down the Tsangpo River Gorge, Southeastern Tibet[J]. Quaternary Research, 2004, 62(2): 201-207.
DOI
URL
|
[8] |
施雅风, 郑本兴, 苏珍. 第四纪冰川、冰期间冰期旋回与环境变化[M]//施雅风.中国冰川与环境. 北京: 科学出版社, 2000: 336-347.
|
[9] |
陈智梁, 孙志明, ROYDEN L H, 等. 四川泸定昔格达组的堰塞湖成因及其意义[J]. 第四纪研究, 2004, 24(6): 614-620.
|
[10] |
刘宇平, MONTGOMERY D R, HALLET B, 等. 西藏东南雅鲁藏布大峡谷入口处第四纪多次冰川阻江事件[J]. 第四纪研究, 2006, 26(1): 52-62.
|
[11] |
曾庆利, 杨志法, 袁广祥, 等. 松宗古湖——藏东南帕隆藏布江末次盛冰期发育的一个冰川堰塞湖[J]. 第四纪研究, 2007, 27(1): 85-92.
|
[12] |
张永双, 赵希涛. 澜沧江云南德钦古水一带第四纪堰塞湖的沉积特征及其环境意义[J]. 地质学报, 2008, 82(2): 262-268.
|
[13] |
张永双, 赵希涛, 胡道功. 滇西北德钦地区金沙江奔子栏古堰塞湖的发现及意义[J]. 地质通报, 2007, 26(8): 970-975.
|
[14] |
姚檀栋, 李治国, 杨威, 等. 雅鲁藏布江流域冰川分布和物质平衡特征及其对湖泊的影响[J]. 科学通报, 2010, 55(18): 1750-1756.
|
[15] |
祝嵩, 吴珍汉, 赵希涛, 等. 用OSL方法确定雅鲁藏布江大拐弯第四纪晚期冰川堰塞湖年龄[J]. 地球学报, 2013, 34(2):246-250.
|
[16] |
韩同林. 西藏活动构造[M]. 北京: 地质出版社, 1987:1-50.
|
[17] |
杨逸畴. 南迦巴瓦峰地区地貌的基本特征和成因[J]. 山地研究, 1984, 2(3): 134-143.
|
[18] |
张文敬, 高登义. 世界第一大峡谷——雅鲁藏布大峡谷科学考察新进展[J]. 山地学报, 1999, 17(2): 99-103.
|
[19] |
张文敬. 南迦巴瓦峰跃动冰川的某些特征[J]. 山地研究, 1985, 3(4): 234-238.
|
[20] |
李翠平, 王萍, 钱达, 等. 雅鲁藏布江大峡谷入口河段最近两期古堰塞湖事件的年龄[J]. 地震地质, 2015, 37(4):1136-1146.
|
[21] |
张沛全, 刘小汉, 孔屏, 等. 雅鲁藏布江大拐弯地区末次冰期以来的冰川活动证据及其构造-环境意义[J]. 地质科学, 2008, 43(3):588-602.
|
[22] |
OWEN L A, DORTCH J M. Nature and timing of Quaternary glaciation in the Himalayan-Tibetan orogen[J]. Quaternary Science Reviews, 2014, 88: 14-54.
DOI
URL
|
[23] |
OWEN L A, FINKEL R C, BARNARD P L, et al. Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by 10Be cosmogenic radionuclide surface exposure dating[J]. Quaternary Science Reviews, 2005, 24(12): 1391-1411.
DOI
URL
|
[24] |
ZHU S, WU Z H, ZHAO X T, et al. Middle-Late Pleistocene glacial lakes in the grand canyon of the Tsangpo River, Tibet[J]. Acta Geologica Sinica, 2012, 86(1): 266-283.
DOI
URL
|
[25] |
黄艳, 袁鹏, 颜志衡. 雅鲁藏布江流域天然径流特征及规律分析[J]. 红水河, 2010, 29(1): 65-69.
|
[26] |
邵兆刚, 孟宪刚, 朱大岗, 等. 青藏高原层状地貌特征及其成因初探[J]. 地学前缘, 2009, 16(6): 186-194.
|
[27] |
韩建恩, 余佳, 邵兆刚, 等. 黄河源晚新生代河湖相沉积与环境[M]. 北京: 地质出版社, 2013:1-5.
|
[28] |
陈建军, 季建清, 龚俊峰, 等. 雅鲁藏布江大峡谷的形成[J]. 地质通报, 2008, 27(4): 491-499.
|
[29] |
HUANG S Y, LIN Y N, CHEN Y G, et al. The implication of elevated lacustrine sediments in the middle reach of the Yarlung-Tsangpo and Nyang River, Tibet[M]// The Cultural History of the Arabs. London: Aurum Press, 2007:5415-5418.
|
[30] |
王富葆, 张厚生. 南迦巴瓦峰地区第四纪地质拾零[J]. 山地研究, 1985, 3(4):321-324.
|
[31] |
CINA S E, YIN A, GROVE M, et al. Gangdese arc detritus within the eastern Himalayan Neogene foreland basin: Implications for the Neocene evolution of the Yalu-Brahmaputra River system[J]. Earth and Planetary Science Letters, 2009, 285(1/2):150-162.
DOI
URL
|
[32] |
ZHANG J Y, YIN A, LIU W C, et al. Coupled U-Pb dating and Hf isotopic analysis of detrital zircon of modern river sand from the Yalu River (Yarlung Tsangpo) drainage system in southern Tibet: Constraints on the transport processes and evolution of Himalayan rivers[J]. Geological Society of America Bulletin, 2012, 124(9/10): 1449-1473.
DOI
URL
|
[33] |
WANG P, SCHERLER D, LIU-ZENG J, et al. Tectonic control of Yarlung Tsangpo Gorge revealed by a buried canyon in Southern Tibet[J]. Science, 2014, 346: 978-981.
DOI
PMID
|
[34] |
KORUP O, MONTGOMERY D R. Tibetan plateau river incision inhibited by glacial stabilization of the Tsangpo gorge[J]. Nature, 2008, 455: 786-789.
DOI
|
[35] |
KORUP O, MONTGOMERY D R, HEWITT K. Glacier and landslide feedbacks to topographic relief in the Himalayan syntaxes[J]. Proceedings of the National Academy of Sciences of the United States of America, 2010, 17(12): 5317-5322.
|
[36] |
BROOKFIELD M E. Evolution of the great river systems of southern Asia during the Cenozoic India-Asia collision: Rivers draining north from the Pamir syntaxis[J]. Geomorphology, 2008, 100(3/4):296-311.
DOI
URL
|
[37] |
王二七, 陈良忠, 陈智樑. 在构造和气候因素制约下的雅鲁藏布江的演化[J]. 第四纪研究, 2002, 22(4):365-373.
|
[38] |
季建清, 钟大赉, 丁林, 等. 雅鲁藏布大峡谷地质成因[J]. 地学前缘, 1999, 6(4): 231-235.
|