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首页> 外文期刊>Anais da Academia Brasileira de Ciencias >Analysis of tectonic-controlled fluvial morphology and sedimentary processes of the western Amazon Basin: an approach using satellite images and digital elevation model
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Analysis of tectonic-controlled fluvial morphology and sedimentary processes of the western Amazon Basin: an approach using satellite images and digital elevation model

机译:亚马逊河流域西部构造控制的河流形态和沉积过程分析:使用卫星图像和数字高程模型的方法

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An investigation of the tectonic controls of the fluvial morphology and sedimentary processes of an area located southwest of Manaus in the Amazon Basin was conducted using orbital remote sensing data. In this region, low topographic gradients represent a major obstacle for morphotectonic analysis using conventional methods. The use of remote sensing data can contribute significantly to overcome this limitation. In this instance, remote sensing data comprised digital elevation model (DEM) acquired by the Shuttle Radar Topographic Mission (SRTM) and Landsat Thematic Mapper images. Advanced image processing techniques were employed for enhancing the topographic textures and providing a three-dimensional visualization, hence allowing interpretation of the morphotectonic elements. This led to the recognition of main tectonic compartments and several morphostructural features and landforms related to the neotectonic evolution of this portion of the Amazon Basin. Features such as fault scarps, anomalous drainage patterns, aligned ridges, spurs and valleys, are expressed in the enhanced images as conspicuous lineaments along NE-SW, NW-SE, E-W and N-S directions. These features are associated to the geometry of alternated horst and graben structures, the latter filled by recent sedimentary units. Morphotectonic interpretation using this approach has proven to be efficient and permitted to recognize new tectonic features that were named Asymmetric Ariaú Graben, Rombohedral Manacapuru Basin and Castanho-Mamori Graben.
机译:利用轨道遥感数据,对亚马逊河流域马瑙斯西南部地区河流形态和沉积过程的构造控制进行了研究。在该区域,低地形梯度代表了使用常规方法进行形态构造分析的主要障碍。遥感数据的使用可以大大克服这一限制。在这种情况下,遥感数据包括由航天飞机雷达地形任务(SRTM)和Landsat专题测绘仪图像获取的数字高程模型(DEM)。先进的图像处理技术被用于增强地形纹理并提供三维可视化效果,因此可以解释构造构造元素。这导致人们认识到主要构造区室以及与亚马逊盆地这一部分新构造演化有关的一些形态构造特征和地貌。在增强图像中,沿NE-SW,NW-SE,E-W和N-S方向的明显线条表现出诸如断层陡坡,异常排水模式,对齐的山脊,山脊和山谷等特征。这些特征与交替的霍斯特和格斗结构的几何形状有关,后者由最近的沉积单元填充。使用这种方法的形态构造解释已被证明是有效的,并允许识别名为不对称AriaúGraben,Rombohedral Manacapuru盆地和Castanho-Mamori Graben的新构造特征。

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