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Source parameters of the 2011 Yellow Sea earthquake (ML 5.3): Different features from earthquakes on the Korean Peninsula

机译:2011年黄海地震(ML 5.3)的震源参数:与朝鲜半岛地震不同的特征

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A moderate earthquake of magnitude ML 5.3 occurred in the Yellow Sea on January 12, 2011. We estimated the source parameters and found that the quake was a shallow strike-slip fault event with a moment magnitude of 4.6. The stress drop of this event, 1.2-2.0 MPa, is lower than that of moderate earthquakes inland and at the eastern offshore of the Korean Peninsula, and also that of the typical value for shallow intraplate earthquakes. A stronger event (M ~ 6) in the southern Yellow Sea in 1984 was previously reported to have a low stress drop. Therefore the low stress drop is probably characteristic of earthquakes in the Yellow Sea region. We found that aftershocks of the 2011 Yellow Sea event, with magnitudes greater than 2, occurred for about 5 days, while similar-sized aftershocks of some inland earthquakes of the Korean Peninsula continued for several hours only. The lower stress drop and greater active aftershocks in the Yellow Sea region might reflect a different tectonic setting from that on the Korean Peninsula.
机译:2011年1月12日,黄海发生了ML 5.3级中度地震。我们估算了震源参数,发现该地震是一个浅层走滑断层事件,矩震级为4.6。该事件的应力降为1.2-2.0 MPa,低于内陆和朝鲜半岛东部近海的中度地震的应力降,也低于浅板内地震的典型值。先前有报道称,1984年在黄海南部发生的一次强事件(M〜6)具有较低的应力降。因此,较低的应力降可能是黄海地区地震的特征。我们发现,2011年黄海事件余震强度大于2,发生了约5天,而朝鲜半岛内陆地震的类似规模余震仅持续了几个小时。黄海地区较低的应力下降和较大的余震活动可能反映了与朝鲜半岛不同的构造环境。

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