Investigating Structural and Tectonic Evolution of Central Afghanistan Using Remote Sensing and Gravity Data

S. Rustami, N. Saadi, E. Aboud, K. Yonezu, Koichiro Watanabe
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引用次数: 7

Abstract

This study used an integrated approach to investigate geological structure and tectonic evolution in Central Afghanistan. Several image processing techniques have been separately and simultaneously applied to data obtained from Landsat Enhanced Thematic Mapper Plus (ETM+) and Digital Elevation Models (DEM) to constrain the geological structure of the study area. Satellite images were combined with Gravity data to better understand 3D geology in the area. Analysis and interpretation of the extracted lineaments indicate that the Central Afghanistan area is controlled by two main fault systems, trending NE and EW. The two trends represent the remnants of reactivated structures that formed under the stress regimes generated during the tectonic evolution of Central Afghanistan. Gravity data indicate a NE trending basin. A two- dimensional (2D) schematic model shows that the basin deepens in the central area and gradually shallows towards the edges. The integration of the results gave insight into the tectonic evolution of the Central Afghanistan area and the adjacent areas.
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利用遥感和重力资料研究阿富汗中部构造和构造演化
本研究采用综合方法研究了阿富汗中部的地质构造和构造演化。利用Landsat Enhanced Thematic Mapper Plus (ETM+)和Digital Elevation Models (DEM)获得的数据分别和同时应用了几种图像处理技术,以约束研究区域的地质结构。卫星图像与重力数据相结合,以更好地了解该地区的三维地质情况。对提取剖面的分析和解释表明,阿富汗中部地区受北东向和东西向两大断裂体系控制。这两个趋势代表了在阿富汗中部构造演化期间产生的应力制度下形成的重新激活的构造的残余。重力资料显示为北东向盆地。二维(2D)图解模型显示,盆地在中心区域逐渐变深,向边缘逐渐变浅。综合研究结果,对阿富汗中部及邻近地区的构造演化有了深入的认识。
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