高分辨率的运动构造模型,覆盖了西藏北部2021年m7.4级地震160公里长的地表破裂

Jing Liu-Zeng , Wenqian Yao , Xiaoli Liu , Yanxiu Shao , Wenxin Wang , Longfei Han , Yan Wang , Xianyang Zeng , Jinyang Li , Zijun Wang , Zhijun Liu , Hongwei Tu
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引用次数: 8

摘要

2021年5月22日,中国青海马多发生的MW 7.4地震提供了一个难得的机会,在极端海拔和天气条件下应用现代无人机(UAV)摄影方法来成像偏远西藏地震相关地表变形的地表破裂和近场效应。在主震发生后的几天内获得了高分辨率的航空照片。与此事件相关的复杂地表破裂模式以3-6 cm分辨率全面覆盖。这是青藏高原内部的地震破裂首次被如此高分辨率的图像全面、系统地捕获,具有前所未有的详细程度,覆盖了整个长度。事实证明,该数据集在记录细微和瞬态破裂特征方面很有价值,例如显著的鼹鼠轨迹和开口裂缝,这些特征在同震中普遍存在,但在随后的夏季风暴季节中退化。这样的高质量图像还有助于高保真地记录地表破裂带的裂缝(本文的补充),与断层如何破裂到地表有关的模式,以及断层外损伤的分布。结合其他地面测绘工作,这些数据将在接下来的几个月里进行分析,以更好地了解与断层带流变学、破裂动力学和断层界面摩擦特性相关的地震破裂力学。
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High-resolution structure-from-motion models covering 160 km-long surface ruptures of the 2021 MW 7.4 Madoi earthquake in northern Qinghai-Tibetan Plateau

The 22 May 2021 MW 7.4 Madoi, Qinghai, China earthquake presented a rare opportunity to apply the modern unmanned aerial vehicle (UAV) photography method in extreme altitude and weather conditions to image surface ruptures and near-field effects of earthquake-related surface deformations in the remote Tibet. High-resolution aerial photographs were acquired in the days immediately following the mainshock. The complex surface rupture patterns associated with this event were covered comprehensively at 3–6 cm resolution. This effort represents the first time that an earthquake rupture in the interior of the Qinghai-Tibetan Plateau has been fully and systematically captured by such high-resolution imagery, with an unprecedented level of detail, over its entire length. The dataset has proven valuable in documenting subtle and transient rupture features, such as the significant mole-tracks and opening fissures, which were ubiquitous coseismically but degraded during the subsequent summer storm season. Such high-quality imagery also helps to document with high fidelity the fractures of the surface rupture zone (supplements of this paper), the pattern related to how the faults ruptured to the ground surface, and the distribution of off-fault damage. In combination with other ground-based mapping efforts, the data will be analyzed in the following months to better understand the mechanics of earthquake rupture related to the fault zone rheology, rupture dynamics, and frictional properties along with the fault interface.

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