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首页> 外文期刊>Remote Sensing of Environment: An Interdisciplinary Journal >Application of high-resolution, interferometric DEMs to geomorphic studies of fault scarps, fish lake valley, Nevada-California, USA
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Application of high-resolution, interferometric DEMs to geomorphic studies of fault scarps, fish lake valley, Nevada-California, USA

机译:高分辨率干涉测量DEM在美国内华达州加利福尼亚鱼湖谷断层陡峭地貌研究中的应用

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Recent developments in interferometric radar remote sensing provide a method for deriving detailed topographic and slope information for fault-scarp detection. In October 1996, the airborne TOPSAR instrument [IEEE Trans. Geosci. Remote Sens., 30 (1992) 933] was flown over southwest Nevada and east-central California. Topography calculated from TOPSAR data are in the form of a high-resolution (5-m spatial grid) digital elevation model (DEM). In this study, we focus upon the large, steep fault scarps that cut alluvium and alluvial fans in Fish Lake Valley, east of the White Mountains of Nevada-Calilornia. A series of topographic profiles extracted from the DEM reveal that the larger fault scarps are greater than 40 m in height and that the average midsection slope angle for all measured scarps is approximately 23°. These large scarps are the product of multiple offsets rather than a single event. Other relevant geomorphic features present in the digital topography include splays and benches along the main fault, levees, cutbanks, gullies incising fault scarp slopes, shutterridges, offset drainage, and small normal faults with scarp heights of only 4-6 m. Field work corroborated general geomorphologic landforms, confirmed fault-scarp morphometry, and aided the evaluation of the accuracy of the DEM. We are also able to assess fault segmentation models that divide the Fish Lake Valley fault zone (FLVFZ) into discrete segments based upon surface-rupture characteristics.
机译:干涉式雷达遥感技术的最新发展提供了一种导出详细地形和坡度信息以进行断层陡坡检测的方法。 1996年10月,机载TOPSAR仪器[IEEE Trans。 Geosci。 Remote Sens。,30(1992)933]飞越内华达州西南部和加利福尼亚中东部。根据TOPSAR数据计算出的地形是高分辨率(5米空间网格)数字高程模型(DEM)的形式。在这项研究中,我们着眼于在内华达州-加利福尼亚州怀特山以东的鱼湖谷中切断冲积层和冲积扇的大型陡峭断层陡坡。从DEM提取的一系列地形图表明,较大的断层陡坡的高度大于40 m,并且所有测得的陡坡的平均断面平均倾斜角约为23°。这些巨大的缺口是多个偏移量而不是单个事件的产物。数字地形中存在的其他相关地貌特征包括沿主要断层的八角形和台阶,堤防,堤岸,切碎陡坡的沟壑,沟渠,偏移排水和陡峭的仅4-6 m高度的小型正常断层。野外工作证实了一般的地貌地形,证实了断层-陡峭形态,并有助于评估DEM的准确性。我们还能够评估断层分割模型,该模型根据表面破裂特征将鱼湖谷断层带(FLVFZ)分为离散段。

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