喜马拉雅西北克什米尔盆地北部Balapur断层的磁化分布和磁化率反演

Ayaz Mohmood Dar, Syed Kaiser Bukhari
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引用次数: 0

摘要

在喜马拉雅西北部克什米尔盆地北部地区进行了地磁测量,以计算Balapur断层的总磁场强度和地下约束条件。发现-0.020 SI至0.001SI的磁化率指数与Balapur断层的走向有关。此外,相关Gulmarg断层的磁化率指数记录为-0.01SI至0.001 SI。本研究表明,Balapur断层在整个走向中产生了发育良好的磁约束。三维反演模型表明,克什米尔北部的巴拉普尔断层具有足够的地下应变特征,可能导致高地震强度。在观察到的数据库和预测的数据库之间几乎没有变化,并且分析记录了20次迭代的0.002的准确度因子。研究表明,地磁测量在基于磁化因子了解地下断层特征方面非常有用。
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Magnetization distribution and susceptibility inversions of the Balapur fault in the northern region of Kashmir basin, NW Himalaya

Ground magnetic surveys were carried out in the northern region of the Kashmir basin, NW Himalaya to calculate the total magnetic intensities and subsurface constraints at the Balapur fault. The susceptibility index of -0.020 SI to 0.001SI was found associated with the strike of the Balapur fault. Further, the susceptibility index of the associated Gulmarg fault was recorded as -0.01SI to 0.001 SI. The present study implies that the Balapur fault has produced well-developed magnetic constraints throughout its strike. The 3D inversion modeling implies that the Balapur fault in north Kashmir has developed enough subsurface strain features and can lead to high earthquake intensity. Little or no variation was found between the observed and predicted databases and the analysis recorded an accuracy factor of 0.002 with 20 iterations. The study suggests that ground magnetic surveys are very useful in understanding the subsurface fault characteristics based on the Magnetization factor.

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