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Forecasting seismic activity rates in northwest Himalaya through multivariate autoregressive forecast of seismicity algorithm

机译:地震活动度的多元自回归预测预报喜马拉雅西北部地震活动率

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In this study, a model based on multivariate autoregressive forecast of seismicity (MARFS) algorithm is adopted to forecast seismic activity rates in northwest Himalaya, using the compiled homogenized moment magnitude (MW) based catalogue. For this purpose, each source zone delineated by Yadav et al. (Pure Appl Geophys 170:283a??295, 2012) is divided into a spatial grid interval of 0.5?°a????a??0.5?° while the entire catalogue span (1975a??2010) is segregated into six time periods/grids to estimate seismic activity rates spatially and temporally. These seismic activity rates which are estimated from spatial density map of hypocenters exhibit high values in Chaman Fault (Zone 1), Hindukush-Pamir region (Zone 3) and the mega thrust systems, i.e., Main Central Thrust, Main Boundary Thrust and Himalayan Frontal Thrust (Zone 4). Then, the seismic activity rates during 2011a??2016 could be forecasted by extrapolating (through auto-regression procedure) those observed for previous time periods. The forecast seismic activity rates are estimated within the values of 0 and 7.57 with high values primarily observed in Hindukush-Pamir region of Zone 3 and the gently north-dipping thrust fault systems (Main Central Thrust, Main Boundary Thrust, Himalayan Frontal Thrust) of Zone 4. Finally, the associated area under the curve of receiver operating characteristics graph suggests the superiority of forecasting model with respect to random prediction, whereas results of the data-consistency test, i.e., N test of our model, exhibit consistency in between the observed and simulated likelihoods. Moreover, the hypothetical t test performed in between the spatial grids of forecast seismic activity rates and observed seismic activity rates confirms that the former is consistent with the latter.
机译:在这项研究中,采用基于地震活动的多元自回归预测(MARFS)算法的模型,使用已编译的基于均质矩震级(MW)的目录来预测喜马拉雅西北部的地震活动率。为此,Yadav等人划定了每个源区。 (Pure Appl Geophys 170:283a ?? 295,2012)分为0.5?°a ???? a ?? 0.5?°的空间网格间隔,而整个目录范围(1975a?2010)分为六个时间/网格来估计空间和时间上的地震活动率。根据震源的空间密度图估计的这些地震活动速率在查曼断裂(1区),欣杜库什-帕米尔地区(3区)和巨型逆冲系统(即主要中央推力,主要边界推力和喜马拉雅额叶)中具有很高的值。推力(4区)。然后,可以通过推断(通过自动回归程序)对先前时间段观察到的地震活动率进行预测,从而预测2011a至2016年的地震活动率。预测的地震活动速率估计在0和7.57范围内,其中较高的值主要在3区的Hindukush-Pamir地区和北缓北倾的逆冲断层系统(主要中央逆冲,主要边界逆冲,喜马拉雅额叶逆冲)中观测到。区域4。最后,接收器工作特征图曲线下方的相关区域表明,预测模型相对于随机预测具有优越性,而数据一致性测试(即我们模型的N检验)的结果则显示了两者之间的一致性。观察和模拟的可能性。此外,在预测地震活动率和观测地震活动率的空间网格之间进行的假设t检验证实了前者与后者一致。

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