2023年2月6日土耳其中南部和叙利亚西北部破坏性双重地震:初步观测和分析

P. Mai, T. Aspiotis, T. A. Aquib, Eduardo Valero Cano, D. Castro-Cruz, A. Espindola-Carmona, Bo Li, Xing Li, Jihong Liu, R. Matrau, A. Nobile, K. Palgunadi, Matthieu Ribot, L. Parisi, C. Suhendi, Yuxiang Tang, B. Yalcin, U. Avşar, Y. Klinger, S. Jónsson
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引用次数: 24

摘要

2023年2月6日,叙利亚中南部和西北部发生了两场7.8级和7.6级大地震。在撰写本文时,叙利亚的死亡人数超过5万人,叙利亚的死亡人数超过7200人。第一次主震的震中位于东安纳托利亚断层(EAF)以东约15公里处,第二次大地震(9小时后)发生在东西向Sürgü断层以北约90公里处。余震描述的断层长度分别为~ 350公里和~ 170公里。利用卫星和地震数据对地表断层偏移、时空破裂演化和记录的地面运动进行一阶分析,我们的研究揭示了大面积破坏的原因。第一次事件使EAF两侧破裂,持续了约80秒,并造成了超过6米的地表断层偏移。第二个事件也发生了双边破裂,持续时间约35秒,地表偏移量超过7米。在第一次主震中,水平地面加速度局部达到2g;哈塔伊-安塔基亚地区发生了严重而广泛的震动,震级接近0.5g。这两次地震都具有方向性效应和突然破裂停止的特征,产生了有助于强地震辐射的停止相。位置放大效应进一步加剧了局部的震动。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Destructive Earthquake Doublet of 6 February 2023 in South-Central Türkiye and Northwestern Syria: Initial Observations and Analyses
On 6 February 2023, two large earthquakes with magnitude 7.8 and 7.6 rocked south-central Türkiye and northwestern Syria. At the time of writing, the death toll exceeded 50,000 in Türkiye and 7200 in Syria. The epicenter of the first mainshock was located ∼15 km east of the east Anatolian fault (EAF), the second large earthquake (9 hr later) initiated ∼90 km to the north on the east–west-trending Sürgü fault. Aftershocks delineate fault lengths of ∼350 and ∼170 km, respectively. Using satellite and seismic data for first-order analyses of surface-fault offsets, space–time rupture evolution, and recorded ground motions, our study sheds light on the reasons for the extensive destruction. The first event ruptured the EAF bilaterally, lasted for ∼80 s, and created surface fault offsets of over 6 m. The second event also ruptured bilaterally with a duration of ∼35 s and more than 7 m surface offsets. Horizontal ground accelerations reached locally up to 2g in the first mainshock; severe and widespread shaking occurred in the Hatay-Antakia area with values near 0.5g. Both earthquakes are characterized by directivity effects and abrupt rupture cessation generating stopping phases that contributed to strong seismic radiation. Shaking was further aggravated locally by site-amplification effects.
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