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雅鲁藏布江中游晚更新世古堰塞湖群的时空关系探讨
引用本文:胡海平,冯金良,刘金花,陈锋. 雅鲁藏布江中游晚更新世古堰塞湖群的时空关系探讨[J]. 冰川冻土, 2022, 44(4): 1298-1305. DOI: 10.7522/j.issn.1000-0240.2022.0117
作者姓名:胡海平  冯金良  刘金花  陈锋
作者单位:1.东华理工大学 地球科学学院,江西 南昌 330013;2.中国科学院 青藏高原研究所 青藏高原环境变化与地表过程重点实验室,北京 100101;3.山西财经大学 资源环境学院,山西 太原 030006
基金项目:国家自然科学基金项目(41901002)
摘    要:雅鲁藏布江中游堵江事件多发,探索堵江事件之间的关系对理解河流地貌演化有着重要作用。在中游宽谷地区,众多河流堆积阶地中保存着古堰塞湖相沉积物。前人对林芝地区、泽当宽谷和日喀则宽谷的古湖相沉积进行了较为深入的研究,三个宽谷在晚更新世均发育过古堰塞湖,但三个地区古堰塞湖之间的时空关系仍未可知。在上述基础上,对雅鲁藏布江中游不同河段古堰塞湖的坝体位置、成因、海拔及发育年代等进行总结分析。归纳出在雅鲁藏布江中游宽谷河段分别发育着3个独立的古堰塞湖,成因多为冰川/冰碛物堵江。晚更新世不同河段降水和地貌条件差异,冰川规模变化速率不同,可能导致冰川前进壅塞河道时间不一致;但3个古堰塞湖的消亡时间较为接近,其溃决过程可能存在关联。

关 键 词:雅鲁藏布江  古堰塞湖  堵江事件  时空关系  晚更新世  冰川  
收稿时间:2022-05-10
修稿时间:2022-08-06

Discussion on spatio-temporal relationship of late Pleistocene dammed palaeo-lakes at the middle Yarlung Tsangpo River
Haiping HU,Jinliang FENG,Jinhua LIU,Feng CHEN. Discussion on spatio-temporal relationship of late Pleistocene dammed palaeo-lakes at the middle Yarlung Tsangpo River[J]. Journal of Glaciology and Geocryology, 2022, 44(4): 1298-1305. DOI: 10.7522/j.issn.1000-0240.2022.0117
Authors:Haiping HU  Jinliang FENG  Jinhua LIU  Feng CHEN
Affiliation:1.School of Earth Sciences,East China University of Technology,Nanchang 330013,China;2.Key Laboratory of Tibetan Environment Changes and Land Surface Processes,Institute of Tibetan Plateau Research,Chinese Academy of Sciences,Beijing 100101,China;3.School of Resources and Environment,Shanxi University of Finance and Economics,Taiyuan 030006,China
Abstract:Yarlung Tsangpo River is easily dammed, and the relationship between damming events are important for understanding the evolution of the landform in the valley. Many lacustrine are exposed in the terraces in the middle Yarlung Tsangpo valley. Lacustrine terraces in the broad Mailing, Zetang, and Xigazê valley are studied, which indicated dammed palaeo-lake occurred during late Pleistocene in all three broad valleys. However, the spatio-temporal relationship between three palaeo-lakes remain unknown. Based on previous studies, herein analysis the dam locations, genesis, elevations, and ages of the palaeo-lakes. During late Pleistocene, three independent separate dammed palaeo-lakes happened in the middle Yarlung Tsangpo River. They are Gega palaeo-lake (3 180 m a.s.l.) in the broad Mailing valley, Jêdêxoi palaeo-lake (3 585 m a.s.l.) in the broad Zetang valley, and Dazhuka palaeo-lake (3 811 m a.s.l.) in the broad Xigazê valley and the Dazhuka-Yueju gorge. It’s likely advance of glaciers have dammed the Yarlung Tsangpo River during late Pleistocene. The advance rates of the glaciers are different due to the geomorphological difference and the precipitation decrease from Nyingchi to Xigazê, and the time of dam formation were different. The Gega palaeo-lake was dammed by the Zelunglung Glacier at the entrance of the Yarlung Tsangpo Gorge. The Jêdêxoi palaeo-lake was probably dammed at the entrance of the Gyaca gorge. On the contrast, the Dazhuka palaeo-lake was likely dammed at the outlet of the Dazhuka-Yueju gorge. However, the extinction age of three dammed palaeo-lakes were similar (about 13 ka), indicate strong relationship between the failure events.
Keywords:Yarlung Tsangpo River  dammed palaeo-lake  damming events  spatio-temporal relationship  late Pleistocene  glacier  
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