Interseismic deformation and 3D kinematic reconstruction of the Balapur Fault, NW Himalaya: Insights from InSAR and gravity data

IF 2.7 3区 地球科学 Q2 GEOCHEMISTRY & GEOPHYSICS
Asrar Ahmad Rather , Syed Kaiser Bukhari
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引用次数: 0

Abstract

The Balapur Fault is one of the most studied faults within the Kashmir Basin due to its possible role in future seismicity and its proximity to the population center in the NW Himalaya. This study utilizes the multidisciplinary approach of Persistent Scatterer InSAR and gravity analysis to study the surface kinematics and subsurface characteristics of the fault structure. Over 200 Sentinel-1 scenes acquired in ascending and descending geometries between 2014 and 2023 were analyzed to derive interseismic deformation patterns, yielding mean Line-of-Sight rates ranging from 1 ± 0.3 mm/yr to 2 ± 0.4 mm/yr. LOS data were decomposed into east-west and vertical components, revealing uplift rates of approximately 2 mm/yr in agreement with the known shortening rates. Cross-sectional velocity analyses along the entire fault length (both mapped and inferred) indicate uniform fault activity, although a detailed fault-locking inversion reveals along-strike heterogeneities. Specifically, Monte Carlo simulations integrated within the inversion framework quantify uncertainties in fault parameters and indicate that while most segments lock at depths of 12–13 km, the northern Segment 1 appears to be locked at greater depths (∼16 km), consistent with a deepening décollement observed in the region. Continuous GPS station data from 3 nearby locations is further utilized to cross-validate and calibrate InSAR-derived displacement rates. Gravity data acquisition and processing, including Complete Bouguer anomaly and Total Horizontal Derivative mapping, provide further constraints on the subsurface structure, delineating fault strike and revealing contrasting density gradients. 3D model inversion of the gravity data uncovers three prominent zones of discontinuity corresponding to the main fault and its subsidiary branches, indicating a high dip angle (>60°) and the deep-rooted nature of the fault. This integrated approach enhances our understanding of fault kinematics and locking behavior in the Balapur Fault and demonstrates the utility of combining geodetic and gravimetric methods for comprehensive seismic hazard assessment.
喜马拉雅西北部Balapur断层的震间形变和三维运动学重建:来自InSAR和重力数据的见解
巴拉普尔断层是克什米尔盆地内研究最多的断层之一,因为它可能在未来的地震活动中起作用,而且它靠近西北喜马拉雅地区的人口中心。本研究利用持续散射InSAR和重力分析等多学科方法研究断裂结构的地表运动学和地下特征。在2014年至2023年期间,Sentinel-1在上升和下降几何形状中获得了200多个场景,分析了地震间变形模式,得出平均视线速率为1±0.3 mm/yr至2±0.4 mm/yr。将LOS数据分解为东西分量和垂直分量,揭示了约2 mm/yr的隆升速率,与已知的缩短速率一致。沿整个断层长度的横断面速度分析(包括映射的和推断的)表明,断层活动是均匀的,尽管详细的断层锁定反演揭示了沿走向的非均质性。具体而言,在反演框架内集成的蒙特卡罗模拟量化了断层参数的不确定性,并表明,虽然大多数段在12-13公里的深度锁定,但北部1段似乎在更深的深度(~ 16公里)锁定,这与该地区观测到的不断加深的变宽一致。来自附近3个地点的连续GPS站数据进一步用于交叉验证和校准insar导出的位移率。重力数据的采集和处理,包括完整的布格异常和总水平导数映射,提供了对地下结构的进一步约束,描绘了断层走向,揭示了对比的密度梯度。重力数据的三维模型反演揭示了主断裂及其附属分支对应的三个突出的不连续带,表明断层倾角大(>60°),断层的深根性。这种综合方法增强了我们对Balapur断层运动学和锁定行为的理解,并展示了大地测量和重力测量相结合的综合地震危险性评估方法的实用性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Tectonophysics
Tectonophysics 地学-地球化学与地球物理
CiteScore
4.90
自引率
6.90%
发文量
300
审稿时长
6 months
期刊介绍: The prime focus of Tectonophysics will be high-impact original research and reviews in the fields of kinematics, structure, composition, and dynamics of the solid arth at all scales. Tectonophysics particularly encourages submission of papers based on the integration of a multitude of geophysical, geological, geochemical, geodynamic, and geotectonic methods
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