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首页> 外文期刊>Seismological research letters >Preface to the Focus Section on the 3 September 2016 Pawnee, Oklahoma, Earthquake
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Preface to the Focus Section on the 3 September 2016 Pawnee, Oklahoma, Earthquake

机译:2016年9月3日Pawnee,俄克拉荷马州,地震的重点部分序幕

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The M_w 5.8 Pawnee earthquake occurred at 12:02 UTC on 3 September 2016, local time at 6:02 a.m. on Saturday. It was widely felt throughout Oklahoma and neighboring states. The earthquake occurred near the junction of the two previously mapped faults: Watchorn fault and Labette fault. However, the actual source fault was the previously unmapped Sooner Lake fault (also known as the Pawnee fault). This is the largest earthquake since the 1950s in the instrumental history in Oklahoma. Many recent studies suggest that most earthquakes in Oklahoma since 2009 are induced by wastewater injection (e.g., Ellsworth, 2013; Keranen et dL, 2014; Walsh and Zoback, 2015), and the Pawnee earthquake is potentially the largest injection-induced earthquake that has occurred so far (Yeck et al., 2016).
机译:M_W 5.8 Pawnee地震发生在2016年9月3日的12:02 UTC,当地时间在星期六上午6:02。 在俄克拉荷马州和邻国的广泛感受到。 地震发生在两个先前映射断层的交界处:观察者故障和伐税故障。 但是,实际的源故障是先前未解除的湖泊故障(也称为Pawnee Fault)。 这是自20世纪50年代以来最大的地震,在俄克拉荷马州的乐器史上。 许多最近的研究表明,自2009年以来俄克拉荷马州大部分地震由废水注射诱导(例如,Ellsworth,2013; Keranen et Dl,2014;沃尔斯和Zoback,2015),并且典当地震可能是最大的注射诱导的地震 到目前为止发生(Yeck等,2016)。

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