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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以来的古陶器展开。通过雷达遥感在中国蒙古东部ejin横幅中的雷达遥感

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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:基于雷达遥感和沉积物相分析,本文研究了自60 kA BP(在场之前)以来的东北欧洲横幅环境演变的特征。结论列出如下:(1)天公湖苏格鲁尔湖,天气湖的演变是由断层和区域气候的主导; (2)通过分析旧菊纳湖的矿床,这是一个大约50ka bp的大型出口湖。在中国西北部的温度下,大约是50kA的BP。事件导致这些湖泊收缩。 (3)在南部北部的隆起发生隆起的故障活动,湖泊的水从北左右流出,大约35ka BP,这是逆转到前流动方向。因此,形成了旧的菊花河流风扇。与此同时,少年湖与苏格鲁克湖和去文旧渠道分开。 (4)附近2000年来,Ruoshui River是一条漫步的河流。由于人类活动的强烈影响,绿洲生态系统在最近15年来迅速堕落。

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