首页> 外文期刊>Journal of the Geological Society of India >Morphometric Analysis of Parvati Basin, NW Himalaya: A Remote Sensing and GIS Based Approach
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Morphometric Analysis of Parvati Basin, NW Himalaya: A Remote Sensing and GIS Based Approach

机译:Parvati盆地的形态学分析,NW Himalaya:基于GIS的遥感和GIS方法

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Morphometry is a quantitative approach of analysing linear, areal and relief parameters to understand the role of neotectonic activity in geomorphologic evolution of a river basin. In the present study multi-disciplinary integrated approach using morphometric parameters along with remote sensing and GIS technique have been applied for determining the quantitative parameters indicative of neotectonic activity in the Parvati basin, Higher Himalaya. The lineament pattern observed in the basin shows major trend in NE-SW followed by NW-SE and NNE-SSW directions. The basin is a 6(th) order drainage basin with dominating dendratic - trellis drainage pattern having very strong structural/tectonic control and is in its late youth stage of geomorphic development. Parvati basin shows coarse drainage density with fine texture suggesting more surface runoff and less infiltration in the area. The basin is highly elongated in shape tapering towards the south-west with high susceptibility to erosion with lower peak flow for longer duration. The above observations clearly indicate a tectonic and lithological control over the evolution of drainage pattern of Parvati basin.
机译:形态测量学是一种定量分析线性、面积和地形参数的方法,以了解新构造活动在流域地貌演化中的作用。在本研究中,使用形态测量参数以及遥感和GIS技术的多学科综合方法已被应用于确定指示高喜马拉雅帕尔瓦蒂盆地新构造活动的定量参数。在盆地中观察到的线性构造模式显示出NE-SW方向的主要趋势,然后是NW-SE和NNE-SSW方向。该盆地是一个6级流域,主要的树状-网格排水模式具有很强的结构/构造控制,并处于地貌发育的晚期青年阶段。Parvati盆地的排水密度较粗,质地较细,表明该地区地表径流较多,渗透较少。盆地高度拉长,向西南方向逐渐变细,具有较高的侵蚀敏感性,峰值流量较低,持续时间较长。上述观察清楚地表明,构造和岩性控制着帕瓦蒂盆地排水模式的演化。

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