SCEC/USGS 利用 2019 年里奇克雷斯特地震序列进行的社区应力下降验证研究

A. Baltay, R. Abercrombie, Shanna Chu, T. Taira
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引用次数: 1

摘要

我们利用 2019 年加利福尼亚里奇克雷斯特地震序列介绍了一项社区应力降验证研究,在这项研究中,研究人员受邀使用一个共同的数据集,采用多种方法独立估算可比测量值。应力降是地震破裂时断层上平均剪应力的变化,因此是地震科学中许多地面运动、破裂模拟和震源物理问题的关键参数。频谱应力降通常是通过拟合辐射能量频谱的形状来估算的,但不同研究对单个地震的估算结果可能相差甚远。在这项由美国地质调查局和加州南部/全州地震中心联合发起的社区研究中,我们试图通过对提交的应力降进行定量比较,了解地震应力降的变异性和不确定性来源。公开可用的数据集包括 2019 年里奇奎斯特地震序列两周内的近 13,000 次 M1 至 7 级地震,记录在 1 度范围内的台站上。作为一项社区研究,我们通过研讨会和会议分享研究结果,并邀请所有感兴趣的人随时加入。
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The SCEC/USGS Community Stress Drop Validation Study Using the 2019 Ridgecrest Earthquake Sequence
We introduce a community stress drop validation study using the 2019 Ridgecrest, California, earthquake sequence, in which researchers are invited to use a common dataset to independently estimate comparable measurements using a variety of methods. Stress drop is the change in average shear stress on a fault during earthquake rupture, and as such is a key parameter in many ground motion, rupture simulation, and source physics problems in earthquake science. Spectral stress drop is commonly estimated by fitting the shape of the radiated energy spectrum, yet estimates for an individual earthquake made by different studies can vary hugely. In this community study, sponsored jointly by the U. S. Geological Survey and Southern/Statewide California Earthquake Center, we seek to understand the sources of variability and uncertainty in earthquake stress drop through quantitative comparison of submitted stress drops. The publicly available dataset consists of nearly 13,000 earthquakes of M1 to 7 from two weeks of the 2019 Ridgecrest sequence recorded on stations within 1-degree. As a community study, findings are shared through workshops and meetings and all are invited to join at any time, at any interest level.
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