摘要
哈纳斯湖位于阿尔泰山深处,最大水深188.5m,平均水深122.1m。横断面具典型的箱形形态,在其底部存在现代活动地堑。湖盆的成因是强烈的构造断陷加上山谷冰川的创蚀及终碛垄的堰塞。随着终绩垄被出流下切,湖泊面积变小。
Hanasi Lake, with the maximum depth of 188.5 m and mean depth of 122.1 m, is located in central part of Altay Mountains. The lake profile shows rarely typical box-form and there exists active graben under the floor, implying intense modern fault rift. The lake basin originates from structural fault, glacial erosion and terminal moraine dam. During the last glacial age, the lake area got smaller due to the cutting down of the terminal moraine.
出处
《冰川冻土》
CSCD
北大核心
1993年第4期559-565,共7页
Journal of Glaciology and Geocryology
关键词
哈纳斯湖
冰川作用
湖泊
成因
地形
Hanasi Lake, landform, structural fault, glaciation
