首页> 外文会议>Second Internatioal Conference on Image and Graphics Pt.1, Aug 16-18, 2002, Hefei, China >Paleodrainage evolution since 60 kaB.P. by radar remote sensing in north- eastern Ejin banner, Inner Mongolia of China
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Paleodrainage evolution since 60 kaB.P. by radar remote sensing in north- eastern Ejin banner, Inner Mongolia of China

机译:自60 kaB.P.以来的古排水演变内蒙古额济纳旗东北部的雷达遥感观测

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摘要

Based on radar remote sensing and sediment facies analyzing, this paper studies the features of environmental evolution of North-eastern Ejin Banner since 60 Ka BP(Before Present). The conclusions are listed as follows: (1) The evolution of Gaxunnur Lake, Sugunur Lake, Tian'e Lake is dominated by faults and regional climate; (2) By analyzing deposit of old Juyanze Lake, it is a large outlet lake about 50Ka BP. Just about 50Ka BP, there was a rapid decline of temperature in the Northwestern of China. The events caused those lakes shrinkage. (3) By fault activity arising uplift in the north of old Juyan Lake and depression in the south, the lake's water flowed out from north to south at around 35Ka BP, which is reversed to the former flow direction. So, old Juyanze fluvial fan was formed. At the same time, Juyan Lake separated from Sugunur lake and Wentugunr old channel was abandoned. (4) Near 2000 years, Ruoshui River is a wandering river. Due to intense influence of human activities, the oasis ecosystem is rapidly degenerated in recently 15 years.
机译:本文基于雷达遥感和沉积相分析,研究了自60 Ka BP以来东北额济纳旗的环境演变特征。得出以下结论:(1)盖逊努尔湖,苏古纳尔湖,天峨湖的演化受断层和区域气候的支配。 (2)通过分析老居延泽湖的沉积物,它是一个约50Ka BP的大型出水湖。大约50Ka BP,中国西北部温度迅速下降。这些事件导致这些湖泊萎缩。 (3)由于断裂活动在旧居延湖北部隆升而在南部凹陷,湖水在35Ka BP左右从北向南流出,与原流向相反。因此,形成了旧的Juyanze河流风扇。与此同时,与Sugunur湖分隔开的Juyan湖和Wentugunr旧河道被废弃了。 (4)近2000年,若水河是一条游荡河。由于人类活动的强烈影响,近15年以来,绿洲生态系统迅速退化。

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