Appraisal of Neotectonic Activities in Shadi Kaur Catchment, Pasni, Balochistan-Pakistan

Waseem Khan, Mahnoor Mirwani, Inayat Ullah, Aimal Khan Kasi, Muhammad Ishaq Kakar, Shazia Fareed
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Abstract

The goal of this research is to assess Neotectonic activity in the northern Pasni region of Balochistan-Pakistan. For atotal of 57 drainage sub-basins, four geomorphic parameters were calculated. These include the Factor of asymmetry(FA), Shape of the Basin (SB), Hypsometric Integral (HI), and Length Gradient of the stream (LGS). The Index ofNeotectonic (IN) was computed using a combination of the calculated geomorphic characteristics. The basins were thenclassified as having high, moderate, and low intensities as a result of this indexing. The tectonic strain by majorlineation found between Hoshab fault and NNE trending Nai Rud fault and NNE trending Ghulaman-i-Bent fault,respectively, has influenced the mechanism of current channels geometry, according to the quantitative analysis. TheIN intensities distribution revealed considerable disparities amongst drainage sub basins, indicating variances inNeotectonic activity due to their placement in relation to the study area's fault networks. A total of 8 knick pointsincluding the slope-break and vertical-step, were distinguished within the catchment area depending on the influencingfactors
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俾路支省-巴基斯坦Pasni地区Shadi Kaur流域新构造活动评价
本研究的目的是评估俾路支省-巴基斯坦北部帕斯尼地区的新构造活动。共计算了57个流域子盆地的4个地貌参数。这些参数包括不对称因子(FA)、盆地形状(SB)、半对称积分(HI)和河流长度梯度(LGS)。结合计算得到的地貌特征,计算了新构造指数。然后根据该指数将盆地划分为高、中、低强度。定量分析了Hoshab断裂与NNE向的Nai Rud断裂和NNE向的Ghulaman-i-Bent断裂之间的主线化构造应变对河道几何形态的影响机制。它们的强度分布显示出各流域子盆地之间的差异,表明它们与研究区断裂网络的位置有关,从而导致了新构造活动的差异。根据不同的影响因素,在流域内划分出坡折和垂直台阶等8个断裂点
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