基于数字高程模拟和二维重力正演的巴基斯坦哈扎拉地区Thandiani至Boi地区地表地壳研究

U. Khan, F. Khan, Tahirinandraina Prudence Rabemaharitra, Malik Arsalan, O. Abdul-Rahim, Inayat Ur Rahman
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引用次数: 1

摘要

重力资料表明,地壳结构、地壳密度(成分)与地表上升之间存在规律性的关系。利用地理信息系统(GIS)的数字高程模型(dem)和重力数据的二维正演模拟相结合的方法,圈定地表和地下地质构造特征,计算地壳和沉积/元沉积楔的厚度变化,为实现主要目标提供了最好的结果。在构造上,研究区位于小喜马拉雅山脉,在一定程度上位于亚喜马拉雅山脉,更具体地说,位于哈扎拉克什米尔构造带的西翼。利用点高法在XYZ坐标下积累地形数据,并将dem的生成、处理、解释和可视化过程定向到surf -15和ArcGIS软件中。明确提出了地表地质构造的dem可视化方法。采用Scintrex CG-5型重力仪对单等高线模式下的重力站进行了量化。对采集到的重力数据进行标准化校正处理,利用重力剖面进行二维正演模拟,利用2.4 g/cm3的布格密度计算布格异常图和重力模型,利用布格异常和重力模型对地下构造进行圈定。总之,本研究为地表和地下地质构造可视化提供了验证。数字高程模型提供了区域地表地质构造的防御性预测。重力模型在基底内划分出一系列具有密度边界的地层单元。重力模型还表明,在Thandiani地区,沉积/变质沉积楔体厚度为11.48 km,在Boi地区,厚度拉长至约14.43 km。Thandiani和Boi地区地壳总厚度分别为49.53 km和52.43 km。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Surface and Crustal Study Based on Digital Elevation Modeling and 2-D Gravity Forward Modeling in Thandiani to Boi Areas of Hazara Region, Pakistan
Gravity data indicates that there is a regular relation between crustal structure, crustal density (composition), and surface ascension. In order to delineate surface and subsurface geological structure features, and to calculate the thickness variation of the crust and sedimentary/metasedimentary wedges, integrated approach of Geographic Information System (GIS) i.e. digital elevation models (DEMs) and two-dimensional forward modeling of gravity data were utilized, which provide the best results for the primary objectives. Tectonically, the study area lies in the Lesser Himalayas as well as to an extent in the sub-Himalaya, more concretely in the western limb of Hazara Kashmir Syntaxis. Topographic data was accumulated in XYZ coordinates utilizing point heights method, and DEMs generation, manipulation, interpretation, and visualization process were directed to surfer-15 and ArcGIS software. Determinately the visualization of surface geological structure in the form of DEMs were proposed. The gravity stations in single contour mode have been quantified by using Scintrex CG-5 gravity meter. The collected gravity data was processed by standardizing corrections, two-dimensional forward modeling along with gravity profile were utilized and bouguer anomaly map and gravity model was computed utilizing bouguer density of 2.4 g/cm3, where the subsurface structures are demarcated by the bouguer anomaly and gravity model. In summary this research has allowed the validation of surface and subsurface geological structure visualization. Digital elevation models provide a defensive prediction of the geological structure of the regional surface. The gravity model demarcated a series of stratigraphic units with density boundaries within the basement. The gravity model also suggests that the thickness of sedimentary/metasedimentary wedge in Thandiani area is 11.48 km and in Boi area, the thickness elongates to about 14.43 km. The total thickness of crust in Thandiani and Boi area is 49.53 km and 52.43 km respectively.
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