Digital elevation model-based lineament analysis of the Zindapir anticline, Sulaiman fold-and-thrust belt, Pakistan

IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY Geological Journal Pub Date : 2024-05-19 DOI:10.1002/gj.4977
Saif-Ur-Rehman K. Jadoon, Lin Ding, Ishtiaq A. K. Jadoon, Syed Saqib Razzaq, Mohsin Javed, Saifullah Afridi, Muhammad Asfandyar Khan, Muhammad Qasim, Fulong Cai
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Abstract

The N-S oriented Zindapir anticline is an eastward verging mega-structure (~130 km along and ~40 km across the strike) in the eastern Sulaiman fold-and-thrust belt on the western margin of the Indian Plate in Pakistan. In this study, we carried out a lineament analysis of the anticline based on shuttle radar topographic mission (SRTM) images and digital elevation model (DEM) data to demonstrate the application of this technique for modelling of the fractured reservoirs. We used shaded relief images, variations in the vertical exaggeration, sun and azimuth angles to enhance the DEM data and structures in the area. Stereographic projections indicated that the anticline is an upright, asymmetrical, gentle, doubly plunging and east-vergent fold. The synthesized lineament map of the fractures indicates a total of 402 fractures across the Zindapir anticline. A total of 204 and 198 fractures were observed in the eastern and western limbs, respectively. Statistical analysis portrayed that the lineaments of the majority of fractures followed northwest-southeast (NW-SE) and west-northwest—east-southeast (WNW-ESE) trends. These are oblique or transverse to the fold axis and could be interpreted as shear and tensional fractures related to drag and compression along the western boundary of the Indian Plate. Our study provides an example of lineament analysis for structural characterization and modelling of fractured reservoirs in a collision-mountain setting.

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基于数字高程模型的巴基斯坦苏莱曼褶皱推覆带津达皮尔反斜线形分析
N-S 向的津达比尔反斜线是巴基斯坦印度板块西缘东部苏莱曼褶皱-推覆带中一个向东延伸的特大构造(沿走向约 130 千米,横跨走向约 40 千米)。在本研究中,我们根据穿梭雷达地形图(SRTM)图像和数字高程模型(DEM)数据对该反斜线进行了线形分析,以展示该技术在断裂储层建模中的应用。我们利用阴影浮雕图像、垂直夸度变化、太阳和方位角来增强该地区的 DEM 数据和结构。立体投影显示,该反斜线是一个直立、不对称、平缓、双垂和东向的褶皱。断裂综合线状图显示,整个津达皮尔反斜线上共有 402 条断裂。在东翼和西翼分别观测到 204 条和 198 条断裂。统计分析表明,大多数断裂的走向呈西北-东南(NW-SE)和西-西北-东-东南(WNW-ESE)走向。这些断裂与褶皱轴线呈斜向或横向,可解释为与印度板块西部边界的拖拽和压缩有关的剪切和张拉断裂。我们的研究提供了一个线状分析的实例,用于碰撞山地环境中断裂储层的构造特征描述和建模。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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