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Probabilistic Assessment of Earthquake Recurrence in Northeast India and Adjoining Regions

机译:印度东北部及邻近地区地震复发的概率评估

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摘要

Northeast India and adjoining regions (20°–32° N and 87°–100° E) are highly vulnerable to earthquake hazard in the Indian sub-continent, which fall under seismic zones V, IV and III in the seismic zoning map of India with magnitudes M exceeding 8, 7 and 6, respectively. It has experienced two devastating earthquakes, namely, the Shillong Plateau earthquake of June 12, 1897 (M w 8.1) and the Assam earthquake of August 15, 1950 (M w 8.5) that caused huge loss of lives and property in the Indian sub-continent. In the present study, the probabilities of the occurrences of earthquakes with magnitude M ≥ 7.0 during a specified interval of time has been estimated on the basis of three probabilistic models, namely, Weibull, Gamma and Lognormal, with the help of the earthquake catalogue spanning the period 1846 to 1995. The method of maximum likelihood has been used to estimate the earthquake hazard parameters. The logarithmic probability of likelihood function (ln L) is estimated and used to compare the suitability of models and it was found that the Gamma model fits best with the actual data. The sample mean interval of occurrence of such earthquakes is estimated as 7.82 years in the northeast India region and the expected mean values for Weibull, Gamma and Lognormal distributions are estimated as 7.837, 7.820 and 8.269 years, respectively. The estimated cumulative probability for an earthquake M ≥ 7.0 reaches 0.8 after about 15–16 (2010–2011) years and 0.9 after about 18–20 (2013–2015) years from the occurrence of the last earthquake (1995) in the region. The estimated conditional probability also reaches 0.8 to 0.9 after about 13–17 (2008–2012) years in the considered region for an earthquake M ≥ 7.0 when the elapsed time is zero years. However, the conditional probability reaches 0.8 to 0.9 after about 9–13 (2018–2022) years for earthquake M ≥ 7.0 when the elapsed time is 14 years (i.e. 2009).
机译:印度东北及毗邻地区(北纬20°–32°和东经87°–100°)极易遭受印度次大陆的地震灾害的危害,该次大陆属于印度地震分区图的V,IV和III级地震带其大小M分别超过8、7和6。它经历了两次毁灭性的地震,分别是1897年6月12日的西隆高原地震(M w 8.1)和1950年8月15日的阿萨姆邦地震(M w 8.5) )在印度次大陆造成了巨大的生命和财产损失。在本研究中,借助三个概率模型,即威布尔,伽玛和对数正态,借助地震目录,估计了在指定时间间隔内M≥7.0级地震发生的概率。时间范围是1846年至1995年。最大似然法已用于估算地震灾害参数。估计似然函数的对数概率(ln L),并将其用于比较模型的适用性,并且发现Gamma模型最适合实际数据。在印度东北部地区,此类地震的样本平均间隔估计为7.82年,魏布尔,伽玛和对数正态分布的预期平均值分别估计为7.837、7.820和8.269年。自该地区上次地震(1995)发生以来,M≥7.0级地震的估计累积概率在大约15-16年(2010-2011年)之后达到0.8,在大约18-20年(2013-2015年)之后达到0.9。在经过时间为零年的M≥7.0地震中,在所考虑的区域中,在大约13-17年(2008-2012年)之后,估计的条件概率也达到0.8至0.9。但是,当经历的时间为14年(即2009年)时,对于M≥7.0的M约7.0级地震,条件概率在大约9-13年(2018-2022年)后达到0.8至0.9。

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