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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
SO NGZO NG LAKE:AN ICE-DAMM ED LAKE OF LAST GLAC IAL M AX M UM IN PURLUNG TSANGPO RIVER,SOUTHEAST TIBET
【作者】 曾庆利; 杨志法; 袁广祥; 尚彦军; 张路青; 赵希涛;
【Author】 Zeng Qingli Yang Zhifa Yuan Guangxiang Shang Yanjun Zhang Luqing Zhao Xitao (Key Laboratory of Engineering Geomechanics,Institute of Geology and Geophysics,Chinese Academy of Sciences,Beijing 100029)
【机构】 中国科学院地质与地球物理研究所工程地质力学重点实验室;
【摘要】 青藏高原东南部帕隆藏布江松宗地区晚更新世期间发生了一次可以识别的支谷冰川阻江形成冰川堰塞湖——松宗古湖的事件。松宗滑坡处的湖相沉积剖面厚度≥88m,其中厚达18.33m并具湖相沉积代表性的连续粉质粘土层底部和顶部的光释光年龄分别为22.5±3.3kaB.P.和16.1±1.7kaB.P.,属末次盛冰期。松宗滑坡处河谷两侧冰碛台地与湖相沉积的接触关系和空间特征指示该湖相沉积与末次盛冰期董曲支谷冰川阻塞帕隆藏布江有关。湖相地层的剖面沉积特征揭示出这个冰川堰塞湖可能贯穿于整个末次盛冰期,但整个帕隆藏布并没有形成统一的山谷冰川。
【Abstract】 An distinguashable ice-dammed lake formed during the Late Pleistocene at the Purlung Tsangpo River,a main downstream tributary of the Yarlung Tsangpo River,in the Songzong Basin of southeast Tibet has been recognized The lacustrine deposit,more than 88 meters thick measured by Total Station(TCA2003),is disclosed after the Songzong landslide.The successional silty clay in the profile is 18.33 meters thick,clearly suggesting the formation of a lake The Optical Simulated Luminescence(OSL) ages at the bottom and top of the silty clay layer are 22.5±3.3kaB.P.,16.1±1.7kaB.P.,respectively,indicating that the lacustrine deposits were formed during the Last Glacial Maximum ranging from 25kaB.P.to 15kaB.P.It was discovered by field geological survey that the sediments were deposited in the outside of the moraine terrace of the Songzong Basin Particularly,the high and large moraine terrace is outcropped in the front of the Dongqu Valley,a big tributary ravine at the south bank of the river The Dongqu Valley upstream is one of the modem glacier centers of southeast Tibet The special characteristics of the lacustrine sediment and the ancient lake line in the Songzong Basin indicate that the lacustrine sediment is related to the blocking of the Purlung Tsangpo River by the glacier in Last Glacial Maximum from Dongqu Valley Moreover,the depositing velocity of the lacustrine reaches to 2.29~2.82mm/a,more quickly than other close lakes in Tibet Evidence also shows that the Songzong ice-dammed lake might run through the Last Glacial Maximum.
【Key words】 ice-dammed lake; Optical Simulated Luminescence(OSL) dating; Last Glacial Maximum; Songzong landslide; Purlung Tsangpo river; Southeast Tibet;
- 【会议录名称】 中国科学院地质与地球物理研究所2007学术论文汇编(第七卷)
- 【会议名称】中国科学院地质与地球物理研究所2007学术年会
- 【会议时间】2008-01-01
- 【会议地点】中国北京
- 【分类号】P343.3
- 【主办单位】中国科学院地质与地球物理研究所(Institute of Geology and Geophysics,Chinese Academy of Sciences)