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青海湖第四纪晚期沉积地震地层特征分析

Analysis on the Characteristic of Seismic Stratigraphy of Later Quaternary Sediment in Qinghai Lake

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【作者】 王平安芷生常宏王苏民沈吉李小强张毅祥孙千里宋友桂艾莉

【Author】 WANG Ping1,AN Zhi-sheng2,CHANG Hong2,WANG Su-min3,SHEN Ji3,LI Xiao-qiang2,ZHANG Yi-xiang1,SUN Qian-li2,SONG You-gui2,AI Li2(1.South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou,510301;2.Institute of Earth Environment,Chinese Academy of Sciences,Xian,710075;3.Nanjing Institute of geography and Limnology,Chinese Academy of Sciences,Nanjing,210008)

【机构】 中国科学院南海海洋研究所中国科学院地球环境研究所中国科学院南京湖泊与地理研究所

【摘要】 青海湖是我国最大的内陆湖泊,目前的水域面积约4400 km2,流域面积约29660 km2。通过在湖内进行高分辨率浅层剖面探测(GeoPulse),发现不同发育阶段的沉积特征在地震剖面上得到很好的反映。Geopulse高分辨率浅层剖面穿透深度约60 m(分辨率为0.5 m),沉积层序在湖盆中央近水平展布,揭示沉积环境相对稳定,但也有局部的扰动或错断。尤其在南部近岸部位,上表层沉积出现弯曲,说明第四纪的晚近期,青海湖有过新的构造运动。

【Abstract】 Qinghai Lake is the largest inland closed-basin lake in China,with an water area of 4 400 km2 and a drainage area of about 29 660 km2.Based on the geopulse high resolution sub-bottom profile survey,the later quaternary sediment characteristics in the lake are revealed on the sub-bottom profiles clearly.The penetration and resolution of the sub-bottom profiles are 60 m and 0.5 m respectively.The profiles in the basin center present a near level sediment stratum that reveals a stable sedimentary environment of the lake.However,there are also some disturbed sediment layer or small faults in basin boundary,especially,in the south nearshore area of the lake.It suggests that there was neo-tectonic movement in later quaternary in Qinghai lake.

【基金】 国家973项目(2004CB720202)的研究成果
  • 【文献出处】 盐湖研究 ,Journal of Salt Lake Research , 编辑部邮箱 ,2009年01期
  • 【分类号】P539.1
  • 【被引频次】1
  • 【下载频次】332
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