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Recent seismicity rate forecast for North East India: An approach based on rate state friction law

机译:印度东北部近期地震活动率预测:一种基于速率状态摩擦定律的方法

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In this study, we have investigated the association of stress-field disparities through earthquake production rate in both spatially and temporally for Northeast region of India. Here, we have implemented the rate and state dependent friction law for forecasting the seismicity rate over M-w = 5.0 earthquake events during the period 2013-2015. The most valuable input model parameter of forecasting seismicity rate is Coulomb stresses changes (Delta CFF), which promote the seismicity rate. The Delta CFF distributions that exhibit significant stress increase in the close proximity of the mainshock sources are found to be diminished with the inverse of the distance from the fault rupture plane. Basically, background seismicity depends on the Coulomb stress changes. These Coulomb stress changes amplify the background seismicity, so a little change in stress can produce very low or high seismicity rate in areas of high ambient seismicity. In several zones the high seismicity rate is revealed by the dominancy of the low b-value. The observed background seismicity rate lies between the ranges of 0-4.0. The significant b-value is achieved in the range of 0.57-1.54 along with average value of 0.93. We have taken the value of constant consecutive parameters (i.e. A sigma = 0.05 MPa) and constant effective friction coefficient of mu' = 0.4 for all the faults. However, in the forecast model we have obtained the stress perturbations and heterogeneous b-value to infer the reliable result in comparison to reference forecast model for the period of 1963-2012. In this study, we have also adopted the RELM experiment in CSEP testing Centre to verify the consistency of the result related to forecast for the duration of 2013-2015. The statistical test provided the satisfactory result for this study region.
机译:在这项研究中,我们调查了印度东北地区在时空上应力场差异与地震发生率的关系。在这里,我们实施了速率和状态相关的摩擦定律,以预测2013-2015年M-w> = 5.0地震事件的地震活动率。预测地震活动率最有价值的输入模型参数是库仑应力变化(Delta CFF),它可以提高地震活动率。发现在主震源附近应力显着增加的Delta CFF分布随着距断层破裂平面距离的倒数而减小。基本上,背景地震活动性取决于库仑应力的变化。这些库仑应力变化会放大背景地震活动性,因此,应力的微小变化会在高环境地震活动性区域中产生非常低或很高的地震活动率。在几个区域中,低b值的优势表明了高地震活动率。观察到的背景地震活动率介于0-4.0之间。显着的b值在0.57-1.54的范围内,平均值为0.93。对于所有故障,我们采用了恒定连续参数(即σ= 0.05 MPa)和恒定有效摩擦系数mu'= 0.4的值。但是,在预测模型中,与1963-2012年期间的参考预测模型相比,我们获得了应力扰动和非均质b值来推断可靠的结果。在这项研究中,我们还通过了CSEP测试中心的RELM实验,以验证2013-2015年期间与预测相关的结果的一致性。统计检验为该研究区域提供了令人满意的结果。

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