2017 年 8 月 18 日美索不达米亚平原 Al-Refaei 地区发生的地震(4.7 mb)的原因和近期应力机制

Q3 Earth and Planetary Sciences
Ali Ramthan
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引用次数: 0

摘要

根据其地震历史,Al-Refaei 地区被认为是美索不达米亚平原地震活动最频繁的地区之一。根据国际地震中心的数据,该地区曾发生过四次地震群,分别是:2004 年 8 月、2013 年 1 月、2017 年 5 月至 6 月以及 2017 年 8 月:分别为 2004 年 8 月、2013 年 1 月、2017 年 5-6 月和 2017 年 8 月。根据三个震级大于 4 mb 的焦点机制解决方案,对该地区的应力进行了分析。焦点机制的结果表明,研究区域的断层运动呈现反向运动,由压缩力产生。为了确定影响该地区断层的主应力轴的方向,采用了旋转优化法。三条应力轴的方向分别为02°/32°、10°/302°和 80°/136°,分别为 σ1、σ2 和 σ3。阿拉伯板块和伊朗板块之间的碰撞是 Al-Refaei 地区地震活动的主要原因。因此,Al-Refaei 活动断层是该地区大多数地震的罪魁祸首,也是 2017 年 8 月 18 日发生的地震的罪魁祸首。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Cause of the Earthquake (4.7 mb) and Recent Stress Regime Occurring in Al-Refaei Area, Mesopotamian plain, August 18th, 2017
Al-Refaei area is considered one of the highest seismically activity in the Mesopotamian Plain according to its seismic history. Depending on the International seismological Center, four seismic swarms were diagnosed in this area; these are: August 2004, January 2013, May-Jun 2017, and August 2017. Based on three focal mechanism solutions of magnitude greater than 4 mb, the stresses in the area were analysed. The results of focal mechanisms suggest that the faults movements in the study area show reverse movements, which is generated by compression force. To determine the directions of principal stress axes that affecting the faults in the area, the Rotational Optimization method were used. The directions of the three stress axes are: 02°/32°, 10°/302°, and 80°/136° for σ1, σ2, and σ3, respectively. The collision between the Arabian and Iranian plates is the main cause of seismic activity in Al-Refaei area. Therefore, Al-Refaei active fault is responsible for most the earthquakes in the area, and responsible for the earthquake that occurred in August 18th, 2017.
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来源期刊
Iraqi Geological Journal
Iraqi Geological Journal Earth and Planetary Sciences-Geology
CiteScore
1.80
自引率
0.00%
发文量
152
审稿时长
7 weeks
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