首页> 外文期刊>Earth, planets and space: EPS >Coulomb stresses imparted by the 25 March 2007 M_w=6.6 Noto-Hanto, Japan, earthquake explain its 'butterfly' distribution of aftershocks and suggest a heightened seismic hazard
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Coulomb stresses imparted by the 25 March 2007 M_w=6.6 Noto-Hanto, Japan, earthquake explain its 'butterfly' distribution of aftershocks and suggest a heightened seismic hazard

机译:2007年3月25日的M_w = 6.6日本诺托·汉托地震所产生的库仑应力解释了其余震的“蝴蝶”分布并暗示了更大的地震危险

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The well-recorded aftershocks and well-determined Source model of the Noto Hanto earthquake provide an excellent opportunity to examine earthquake triggering associated with a blind thrust event. The aftershock zone rapidly expanded into a 'butterfly pattern predicted by Static Coulomb stress transfer associated With thrust faulting. We found that abundant aftershocks occured where the static Coulomb stress increased by more than 0.5 bars. while few shocks Occurred in the Stress Shadow calculated to extend northwest and Southeast of the Now Hanto rupture. To explore the three-dimensional distribution of the observed aftershocks and the calculated stress imparted by the mainshock, WC further resolved Coulomb stress changes oil file nodal planes of all aftershocks for which focal mechanisms are available. About 75% of the possible faults associated with the moderate-sized aftershocks, Were Calculated to have been brought closer to failure by the mainshock. with the correlation best low apparent fault friction. Out-interpretation is that most of the aftershocks struck oil the steeply dipping source fault and on a conjugate northwest-dipping reverse fault contiguous with the source fault. Since we found that the Coulomb hypothesis works well for the Noto Hanto sequence, we subsequently computed stress changes on the nearby active faults. Although the calculated Stress changes were found to be negligible on the major faults south of the Noto Peninsula, several Short active falults near the epicentral area were calculated to have been brought several bars closer to failure. Thus, the probability of strong shaking in and around the epicentral area may still be high due to the transfer of stress to the adjacent faults by a short blind thrust fault.
机译:记录良好的诺托汉托地震余震和确定的震源模型为检查与盲冲推力事件有关的地震触发提供了极好的机会。余震区迅速扩展成“蝶型”,这是由与推力断层有关的静态库仑应力传递预测的。我们发现大量的余震发生在静态库仑应力增加超过0.5巴的地方。而应力阴影中几乎没有发生过震动,该震动被认为可以扩展到现在汉托破裂的西北部和东南部。为了探索观测到的余震的三维分布和主震施加的计算应力,WC进一步解析了库仑应力,改变了所有具有震源机制的余震的油层结面。据计算,与中等规模余震有关的可能断层中,约有75%被主震带到了更接近破坏的地步。相关性最好,表观断层摩擦低。解释是,大多数余震都是在陡倾源断裂以及与源断裂相邻的共轭西北倾逆断层上发生的。由于我们发现库仑假设对于Noto Hanto序列运行良好,因此我们随后计算了附近活动断层的应力变化。尽管发现在诺托半岛以南的主要断层上计算出的应力变化可以忽略不计,但经计算,震中区域附近的几个短活动断层却使几个条带更接近破坏。因此,由于短的盲冲断层将应力转移到相邻断层,在震中区及其附近发生强烈震动的可能性仍然很高。

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