2022 年 2 月危地马拉 6.2 级中深层地震的断裂面

R. Yani-Quiyuch, L. Asturias, D. Castro
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引用次数: 0

摘要

2022 年 2 月 16 日,危地马拉俯冲带发生了一次中等深度板内地震,震级为 6.2 级,震中位于埃斯昆特拉省西南部。记录到的余震超过 275 次,利用 HypoDD 算法对这些余震进行了重新定位,确定了一个面积约 350 平方公里的断层,大大高于对该震级地震的预期。通过主震中心点的力矩张量以及对最大余震的其他焦点机制的估计,我们可以确定与断层面有关的延伸地震,以及与板坯上部地震有关的压缩地震。该序列区域近年来地震活动频繁。据推测,主震发生在该地区双地震带的下地震层(LSL),引发了该地区原有活动断层的地震活动,同时也引发了上地震层(USL)的地震活动。这些地震层之间的间隔估计为 12.2±5.0 公里。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The rupture plane of the February 2022 Mw 6.2 Guatemala, intermediate depth earthquake
An intermediate depth intraplate earthquake with Mw 6.2 was generated in the Guatemalan subduction zone on 16 February 2022 with epicenter to Southwest of the department of Escuintla. More than 275 aftershocks were registered, which were relocated with the HypoDD algorithm, being able to identify a fault with an area of ~350 km2, which is considerably higher than expected for an earthquake of that magnitude. The moment tensor at the centroid of the main earthquake and the estimation of other focal mechanisms of the largest aftershocks, allowed us to identify extension earthquakes, related to the fault plane, and compression earthquakes that were associated with seismicity on the upper part of the slab. The region of the sequence has presented high seismic activity in recent years. It is proposed that the mainshock nucleated in the lower seismicity layer (LSL) of the double seismicity zone proposed for the region, triggering seismic activity on a pre-existing active fault, also triggering seismic activity in the upper seismicity layer (USL). The separation between these seismicity layers was estimated to be 12.2±5.0 km.
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