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The Geomorphologic Characterization of Qinling Mountain Based on DEM

机译:基于DEM的秦岭山脉立陶宛特征

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The Qinling Mountain plays an important role in the formation and evolution of China continent, which is the North-South divide of China in physical geography. It constitutes three parts: East-Qinling, Central-Qinling and Western-Qinling Mountains. The paper was aimed at analyzing the different geomorphic characteristics based on DEM and the relation between the landforms and geology. Some topographic parameters were calculated, such as mean elevation, summit and base level, local relief and mean slope. The DEM data was the SRTM DEM with spatial resolution of 90m The swath profiles method was used, which the profiles were divided into 5-km -wide segments. For each segment, max, min and mean elevation data of 100-km-long swath were projected onto the profile. Three swath profiles were constructed across the eastern, central and western part through the Qinling Mountains. The results show that: elevation is higher in the west traverse comparing the central and east traverse. The area of granitite by high values of local relief which are related to the deeply incised valleys prevailing in the Taibai Mountain. Lithology and drainage network influence the geomorphology pattern in Qinling Mountain which is the reason that different geomorphology from the south to north.
机译:秦岭山在中国大陆的形成和演变中发挥着重要作用,这是中国南北分裂的物理地理。它构成了三个部分:东秦岭,中央秦岭和西秦岭。本文旨在分析基于DEM的不同地貌特征以及地貌与地质的关系。计算一些地形参数,例如平均高度,峰会和基础水平,局部浮雕和平均斜率。 DEM数据是具有90M的空间分辨率的SRTM DEM,使用SWATH配置文件方法,该方法将曲线分为5公里的段。对于每个段,最大,最小和平均升高数据的100千米长的条件被投影到配置文件上。通过秦岭,在东部,中西部和西部建造了三种斯巴斯档案。结果表明:西部横向比较中央和东部的展开横向升高。由局部救济的高价值的诱饵面积与Taibai Mountain普遍有关的山谷。岩石和排水网络影响了秦岭山脉的地貌模式,这是南北不同地貌的原因。

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