2023 年土耳其双重地震揭示了东安纳托利亚断裂带的复杂性:从余震模式和力矩张量解决方案中获得的启示

Sezim Ezgi Güvercin
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摘要

东安纳托利亚断裂带(EAFZ)是沿安纳托利亚板块和阿拉伯板块边界长达 700 公里的左侧转换断层系统。在地震间歇期,东安纳托利亚断裂带的东段表现出相对均匀的地震活动,而西段则表现出地震间隙、局部震群和广泛的弥漫区。因此,我们对西部和北部地段的几何形状和运动学的了解仍然有限。2023 年 2 月 6 日在主干线上发生的 7.8 级 Kahramanmaraş 地震和在北干线上发生的 7.6 级 Elbistan 地震导致了复杂的余震活动,揭示了这些相对沉寂的地段的性质。在本研究中,为了更好地了解断层的复杂性,我们利用基于深度神经网络的选取器,构建了一个包含 2023 年 2 月 6 日至 2023 年 3 月 30 日期间发生的 ∼32,000 次地震的综合目录。此外,从区域矩张量反演中获得了 170 个 Mw 3.5+ 的震源机制。余震的空间分布显示,大部分余震活动都聚集在断层弯曲处和主要凹陷处。在这些几何形状复杂的断层中,还发现了以前未绘制地图和不活跃的不同长度的次级断层。新的地震学观测结果提供了令人信服的证据,证明卡拉苏河谷沿线存在延伸,埃尔肯内克地段存在压缩,纳勒断层带附近的盆地断层重新活跃,以及普图尔格地段存在持续的浅层地震蠕变。对北部分支沿线地震活动性和震源机制的分析揭示了以前不活跃的断层结构,包括西部的延伸性戈克孙弯道附近和东部的压缩性努尔哈赤断层群。总之,我们揭示了东亚大陆断裂带以前不活跃的地段的复杂性,旨在深入了解东亚大陆断裂带沿线的次级断层和几何不连续性是如何在 2023 年 Türkiye 双重地震中发挥作用的。
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2023 Earthquake Doublet in Türkiye Reveals the Complexities of the East Anatolian Fault Zone: Insights from Aftershock Patterns and Moment Tensor Solutions
The East Anatolian Fault Zone (EAFZ) is a 700-km-long left-lateral transform fault system along the boundary between the Anatolian and Arabian plates. In the interseismic period, the eastern segments of the EAFZ display relatively uniform seismic activity, whereas the western segments exhibit seismic gaps, localized clusters, and extensive diffuse zones. Hence, our understanding of the geometry and kinematics of the western and northern segments remain limited. The occurrences of the 6 February 2023 Mw 7.8 Kahramanmaraş on the main branch and Mw 7.6 Elbistan earthquakes on the northern branch have led to complex aftershock activity shedding light on the nature of these relatively silent segments. In this study, to better understand the complexities of the fault, we constructed a comprehensive catalog of ∼32,000 earthquakes that occurred between 6 February 2023 and 30 March 2023, using a deep-neural-network-based picker. In addition, 170 earthquake source mechanisms with Mw 3.5+ were obtained from regional moment tensor inversion. The spatial distribution of the aftershocks shows that most of the activity clusters around the fault bends and major depressions. Previously unmapped and inactive secondary faults of varying lengths are identified within these geometrical complexities. The new seismological observations provide compelling evidence of extension along the Karasu valley, compression occurring along the Erkenek segment, reactivation of basin faults near the Narlı fault zone and the persistent shallow seismic creep of the Pütürge segment. The analysis of seismicity and earthquake source mechanisms along the northern branch reveals the structures of previously inactive faults, both near the extensional Göksun bend in the west and the compressional Nurhak fault complex in the east. In summary, we illustrate the intricacies of previously quiet segments of the EAFZ and aim to gain a deeper understanding of how secondary faults and geometrical discontinuities along the EAFZ played a role in shaping the 2023 Türkiye doublet earthquakes.
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