中部圣安德烈亚斯断层地震对的时空不对称性:远距离小地震联系的证据

P. Shearer, W. Fan
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引用次数: 0

摘要

我们在1981年至2021年间,沿着圣胡安包蒂斯塔以南的加州圣安地列斯断层100公里的路段确定了51对近同期地震,它们在时间上间隔5-50秒,在空间上间隔5-50公里。这些事件对贯穿整个时间段,通常涉及规模小于2级的事件。对其中42对(82%)来说,较晚发生的地震位于较早发生的地震的西北方向——这种不对称很难用标准的地震触发模型来解释,这表明这些事件之间存在潜在的物理联系。我们探索了这些观察的可能起源,但无法确定一个明确的解释。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Space–Time Asymmetry in Earthquake Pairs along the Central San Andreas Fault: Evidence for Small Earthquake Links at Long Distances
We identify 51 near-contemporaneous earthquake pairs along a 100 km segment of California’s San Andreas fault south of San Juan Bautista between 1981 and 2021 that are separated by 5–50 s in time and 5–50 km in space. The event pairs are found throughout the time period and generally involve events smaller than magnitude 2. For 42 of these pairs (82%), the later earthquake is northwest of the earlier event—an asymmetry that is hard to explain with standard earthquake triggering models and suggests an underlying physical connection between the events. We explore possible origins for these observations but are unable to identify a definitive explanation.
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