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Source characteristics of Peruvian deep focus seismic doublet of November 24, 2015

机译:2015年11月24日秘鲁深度焦点地震双重源特征

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摘要

The Peruvian deep focus seismic doublet of November 24, 2015 is the largest event recorded on the Peru-Brazil border in the last 50 years, with hypocenter depth at 655 km (Mw 7.4) for the first event and 675 km (Mw 7.5) for the second event, both events were separated by a distance of 50 km and by a time of 5 min. There was no damage on the surface, but the earthquake was felt in part of Peru (IV MM in Esperanza Ucayali) and Brazil. The parameters that characterize the seismic source have been obtained from the inversion of teleseismic waveforms. For example, the duration of the rupture process was around 25 s for both events and the rupture velocity was between 2.5 and 2.8 km/s. The source time function is similar for both events: it starts with a small energy release before 10 s and then the greatest energy release between 10 s and 20 s. The focal mechanism is of normal fault type, corresponding to tensional tectonic regime of deep slab in the region.
机译:2015年11月24日的秘鲁深度焦点地震倍感是过去50年来在秘鲁 - 巴西边境上录制的最大活动,持续655公里(MW 7.4)的低刻度深度,为675公里(MW 7.5) 第二次事件,这两个事件都分开了50公里的距离和5分钟的时间。 表面上没有损坏,但秘鲁的一部分(IV MM在Esperanza Ucayali)和巴西的地震中感觉到了地震。 表征地震源的参数已经从迭代波形的反转获得。 例如,两个事件的破裂过程的持续时间约为25秒,并且破裂速度在2.5和2.8km / s之间。 源时间函数对于这两个事件类似:它在10秒之前的小能量释放开始,然后在10 s和20秒之间最大的能量释放。 焦点机制是正常的故障类型,对应于该区域深板的张力构造制度。

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