首页> 外文会议>Geoscience and Remote Sensing Symposium, 2008 IEEE International-IGARSS 2008 >Remote Sensing Analysis of Recent Active Tectonics in Pamir Using Digital Elevation Model: River Profile Approach
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Remote Sensing Analysis of Recent Active Tectonics in Pamir Using Digital Elevation Model: River Profile Approach

机译:基于数字高程模型的帕米尔高原近期活动构造的遥感分析:河流剖面法

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Digital elevation models (DEMs) are key component for computer-based analyses of river profiles, drainage basin as it provides elevation information for the land surface throughout the catchment of the area. During the Cenozoic uplift of Tibetan plateau and surrounding ranges due to India-Eurasia collision, the tectonic processes are interacting with the local random effects (e.g. Landslides, Glaciations and climatic Changes) and are linked with the development of a unique river network in this region. These rivers have distinct patterns and are controlled by different tectonic and climatic regions. Drainage history of the Pamir is related to continental movements of the plates, displacements of the tectonics, regional uplift and erosion of various individual tectonic units. This study focuses on the application of remote sensing techniques in order to show the spatial variation of uplift and deformation along the right bank tributaries of Pyanj (Vanch, Yazgulem, Aksu-Murghab-Bartang, Gunt-Alichur and Shokhdara) and one of the few left bank tributary (Shiveh river) and Pyanj itself. DEM data is used to extract river network in this area. Moreover, slopes and drainage areas are also calculated from Digital Elevation Model. Based on the stream power law, we make area-slope plot so as to derive channel parameters like concavity (??) and steepness (Ks) which are related closely to uplift and deformation. The lineaments and major tectonic features have been digitized from geological maps of the region. The uplift, steepness and hack index maps have been generated by using some specially designed algorithms for this purpose.
机译:数字高程模型(DEM)是基于计算机的河流剖面和流域分析的关键组成部分,因为它为整个集水区的陆地表面提供了高程信息。在印度洋与欧亚大陆碰撞引起的青藏高原及其周边地区新生代隆起期间,构造过程与当地的随机效应(例如滑坡,冰川和气候变化)相互作用,并与该地区独特的河网的发展联系在一起。 。这些河流具有独特的格局,并受不同的构造和气候区域控制。帕米尔(Pamir)的排水历史与板块的大陆运动,构造的位移,区域隆升和各个构造单元的侵蚀有关。这项研究侧重于遥感技术的应用,以显示沿Pyanj(Vanch,Yazgulem,Aksu-Murghab-Bartang,Gunt-Alichur和Shokhdara)右岸支流的隆起和变形的空间变化。左岸支流(Shiveh河)和Pyanj本身。 DEM数据用于提取该区域的河网。此外,坡度和流域面积也可以通过数字高程模型计算得出。基于流功率定律,我们绘制了面积-坡度图,从而得出了与隆起和变形密切相关的诸如凹度(?)和陡度(K s )之类的渠道参数。构造和主要构造特征已从该地区的地质图数字化。为此,使用一些特殊设计的算法生成了隆起,陡度和坡度指数图。

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