四川九寨沟风景区的长海不是冰川堰塞湖而是崩塌型堰塞湖

    Instead of glacier damming lake, Changhai Lake in Jiuzhaigou Resort Area, Sichuan Province, China should be regarded as a damming lake caused by collapse

    • 摘要: 从长海湖堤堆积物的结构、终碛堤缺少上游连续的冰碛层、长海地区成坝时没有冰川作用、终碛堤论无法解释如何形成湖库的机制、53.6万年古老的湖堤与仍处于幼年期的湖泊这种有悖于自然演化规律的现象等方面否定了长海冰川堰塞湖论。长海湖堤堆积物与两侧基岩的岩性相同,具有垂向堆积结构、与崩塌型堰塞湖相同的边坡特征,并有产生崩塌的地质背景和形成湖堤稳定的地质因素,从而确认长海为崩塌型堰塞湖。

       

      Abstract: From the structure of bank accumulations of Changhai Lake and lack of continuous upstream drift sheet in the end moraine bar, in view of the fact that there is no glaciation during the time when the dam is formed, as well as the formation of lake reservoir can’t be interpreted by “end moraine bar” theory and the huge age difference between ancient bank(53.6MAa) and young lake, this paper has denied the conclusion that Changhai Lake in Jiuzhaigou Resort Area, Sichuan Province is a glacier damming lake. Lithology of the bank accumulations and its lateral base rock are basically the same with vertical structure and with similar slope structure of other damming lakes caused by collapse, moreover, the regional geologic background is favorable for collapse and stable bank. It′s concluded that Changhai Lake is a damming lake of collapse cause.

       

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