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首页> 外文期刊>Indian Journal of Geosciences >The 18th September 2011 Sikkim Earthquake (Mw 6.8) and its aftershocks recorded in Adampool Seismic Observatory
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The 18th September 2011 Sikkim Earthquake (Mw 6.8) and its aftershocks recorded in Adampool Seismic Observatory

机译:2011年9月18日锡金地震(Mw 6.8)及其余震记录在Adampool地震台上

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On 18th September 2011, an earthquake of magnitude Mw 6.8 occurred 84 km northwest of Adampool Seismic Observatory near Gangtok, in the mountainous region of northeast India in Sikkim-Nepal border region. The source parameters for this earthquake have been estimated using record of the event in the observatory. The spectral analysis of waveform on transverse component of the three-component seismograms is performed. The estimated seismic moment (Mo), source radius (R), stress drop (Δσ) and magnitude (Mw) for this earthquake are 1.99×10~(19) Nm, 10.17 km, 83.24 bar and 6.8 respectively. The present study elucidates the seismicity of the region before and after the occurrence of mainshock with recorded earthquakes especially also with those events (M< 3.0) that are not recorded by distant observatories of the national network and local seismic network. The data recorded in the observatory for the period before the occurrence of this earthquake do not show any noticeable or anomalous precursory activity close to the mainshock except the background seismicity. To show the variation of seismic moment with corner frequency, source radius and stress drop, 19 well-recorded aftershocks (5.0 > Mw > 2.7) are selected in this study. The estimated seismic moment, source radius and stress drop of these aftershocks range from 1.58 x 1013 Nm to 4.27 x 1016 Nm, 0.24 km to 0.98 km and 0.9 bar to 294.2 bar respectively.
机译:2011年9月18日,在印度东北部锡金-尼泊尔边境地区的甘托克附近,亚当普尔天文台西北84公里处发生了6.8级Mw地震。已使用天文台中的事件记录估算了此次地震的震源参数。进行了三分量地震图横向分量波形的频谱分析。该次地震的估计地震矩(Mo),震源半径(R),应力降(Δσ)和震级(Mw)分别为1.99×10〜(19)Nm,10.17 km,83.24 bar和6.8。本研究阐明了有记录地震的大震发生前后该地区的地震活动,特别是那些国家网络和地方地震网络的遥远观测站未记录的那些地震(M <3.0)。除背景地震活动性外,天文台记录的地震发生前一段时间内的数据没有显示出与主震相近的任何明显或异常的前兆活动。为了显示地震矩随转角频率,震源半径和应力降的变化,本研究选择了19条记录良好的余震(5.0> Mw> 2.7)。这些余震的估计地震矩,震源半径和应力降分别为1.58 x 1013 Nm至4.27 x 1016 Nm,0​​.24 km至0.98 km和0.9 bar至294.2 bar。

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