3D Dynamic Rupture Modeling of the 6 February 2023, Kahramanmaraş, Turkey Mw 7.8 and 7.7 Earthquake Doublet Using Early Observations

A. Gabriel, T. Ulrich, M. Marchandon, J. Biemiller, J. Rekoske
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Abstract

The 2023 Turkey earthquake sequence involved unexpected ruptures across numerous fault segments. We present 3D dynamic rupture simulations to illuminate the complex dynamics of the earthquake doublet. Our models are constrained by observations available within days of the sequence and deliver timely, mechanically consistent explanations of the unforeseen rupture paths, diverse rupture speeds, multiple slip episodes, heterogeneous fault offsets, locally strong shaking, and fault system interactions. Our simulations link both earthquakes, matching geodetic and seismic observations and reconciling regional seismotectonics, rupture dynamics, and ground motions of a fault system represented by 10 curved dipping segments and embedded in a heterogeneous stress field. The Mw 7.8 earthquake features delayed backward branching from a steeply branching splay fault, not requiring supershear speeds. The asymmetrical dynamics of the distinct, bilateral Mw 7.7 earthquake are explained by heterogeneous fault strength, prestress orientation, fracture energy, and static stress changes from the previous earthquake. Our models explain the northward deviation of its eastern rupture and the minimal slip observed on the Sürgü fault. 3D dynamic rupture scenarios can elucidate unexpected observations shortly after major earthquakes, providing timely insights for data-driven analysis and hazard assessment toward a comprehensive, physically consistent understanding of the mechanics of multifault systems.
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利用早期观测数据建立 2023 年 2 月 6 日土耳其卡赫拉曼马拉什 7.8 级和 7.7 级双联地震的三维动态破裂模型
2023 年土耳其地震序列涉及众多断层段的意外断裂。我们展示了三维动态断裂模拟,以揭示地震双曲线的复杂动态。我们的模型受到地震发生后数天内观测数据的制约,能够及时、机械地解释未预见的破裂路径、不同的破裂速度、多次滑动、异质断层偏移、局部强烈震动以及断层系统相互作用。我们的模拟将两次地震联系在一起,与大地测量和地震观测结果相匹配,并调和了区域地震构造、破裂动力学以及由 10 个弯曲倾斜段组成的断层系统的地面运动,该断层系统被嵌入一个异质应力场中。这次威力 7.8 级地震的特点是从一个陡峭的分支断层向后延迟分支,不需要超剪切速度。不同的、双边的 Mw 7.7 地震的非对称动力学可以用异质断层强度、预应力方向、断裂能量和前一次地震的静应力变化来解释。我们的模型解释了其东部断裂的向北偏移以及在 Sürgü 断层上观察到的最小滑动。三维动态断裂情景可以阐明大地震后不久的意外观测结果,为数据驱动的分析和危害评估提供及时的见解,从而对多断层系统的力学原理有一个全面的、物理上一致的了解。
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