首页> 外文期刊>Geomatics,Natural Hazards & Risk >Weibull distribution analysis of precursory time due apparent resistivity anomaly prior to earthquakes in the vicinity of multi-parametric geophysical observatory, Tezpur, India
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Weibull distribution analysis of precursory time due apparent resistivity anomaly prior to earthquakes in the vicinity of multi-parametric geophysical observatory, Tezpur, India

机译:在印度多参数地球物理天文台附近发生地震前视电阻率异常的前介时间视电阻率异常的威布尔分布分析

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The apparent resistivity imaging at multiparametric geophysical observatory (MPGO), Ouguri Hills, Tezpur was carried out since 31st August, 2016 for fixed interval time of 3?days to investigate precursory signature prior to earthquake events. Anomalies in apparent resistivity prior to earthquake events are observed. The anomalies are not influenced by the rainfall activity in the region during the investigation period. We adopt Weibull distribution technique with observed apparent resistivity data to look for and revalidate the observations. The Weibull parameters, i.e. K and m are estimated to be 0.26 and 1.04, respectively. No precise relation between magnitude and earthquake precursory time is found. Simultaneously, an attempt has been made to establish a relation between the earthquake magnitude (M) and precursory time (T) and a relation between the earthquake precursory time (T) and distance of the earthquake (Δ) from the observation point. Weibull probability distribution indicate the probability of an earthquake occurrence exceeds the measure up to 80% (9?days) after the precursory signal is observed. A comparison of probability analysis ascertains a mean precursory time and its standard deviation.
机译:自2016年8月31日以来,在2016年8月31日以来,在2016年8月31日以来,进行了无表情的电阻率成像,以自2016年8月31日为3?天在地震事件前调查前兆签名的固定间隔时间进行。观察到地震事件前表观电阻率的异常。在调查期间,异常不受该地区降雨量的影响。我们采用威布尔分布技术,观察到的明显电阻率数据寻找并重新验证观察。 Weibull参数,即k和m分别估计为0.26和1.04。没有找到幅度和地震前面位时间之间的精确关系。同时,已经尝试建立地震幅度(M)和前身时间(T)之间的关系以及地震前身时间(T)与地震(Δ)之间的关系与观察点之间的关系。威布尔概率分布表明,在观察到前面值信号之后,地震发生的概率超过了高达80%(9?天)的度量。概率分析的比较确定平均前置时间及其标准偏差。

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