Peace River Induced Seismic Monitoring (PRISM) Nodal Seismic Array

Yu Jeffrey Gu, Wenhan Sun, Tai-Chieh Yu, Jingchuan Wang, Ruijia Wang, Tianyang Li, R. Schultz
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Abstract

From 23 November 2022 to 30 November 2022, a sequence of earthquakes with a peak magnitude of ML 5.6 occurred ∼46 km away from Peace River—a vibrant rural community in Alberta, Canada. Broadly felt by residents throughout central Alberta, the ML 5.6 earthquake on 30 November 2022, registers as the second-largest earthquake ever reported in the Western Canada Sedimentary basin and possibly the largest Canadian earthquake induced by human activities. On 6 December 2022, 1 week after the mainshock, the University of Alberta and Alberta Geological Survey jointly installed a circular array of nodal geophones surrounding the seismogenic zone. Over the next 4 months, this quick-response array (nicknamed “Peace River Induced Seismic Monitoring” array, for short PRISM) operated at temperatures as low as −30°C and substantially bolstered the seismic data coverage in this previously undersampled region. Our preliminary array data analysis has detected more than 2000 earthquakes with magnitudes ranging from −1.9 to 5.0 since the initial outbreak in late 2022. Investigations based on earthquake location, focal mechanism, and magnitude jointly reveal distinct earthquake clusters distributed along pre-existing faults from earlier tectonic events. The data recovered from this array offer unique and vital constraints on the tectonic histories and seismic risks of the Peace River region.
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和平河诱发地震监测(PRISM)节点地震阵列
从 2022 年 11 月 23 日到 2022 年 11 月 30 日,在距离加拿大艾伯塔省和平河--一个充满活力的农村社区--46 公里处发生了一系列地震,峰值为 ML 5.6。整个艾伯塔省中部的居民都有广泛的震感,2022 年 11 月 30 日发生的 ML 5.6 级地震是加拿大西部沉积盆地有史以来报告的第二大地震,也可能是人类活动引发的加拿大最大地震。2022 年 12 月 6 日,即主震发生一周后,阿尔伯塔大学和阿尔伯塔地质调查局联合在成震区周围安装了一个环形节点检波器阵列。在接下来的 4 个月里,这个快速反应阵列(昵称为 "和平河诱发地震监测 "阵列,简称 PRISM)在低至 -30°C 的温度下工作,大大加强了这一以前取样不足地区的地震数据覆盖范围。通过对阵列数据的初步分析,我们发现自 2022 年末首次爆发地震以来,共发生了 2000 多次地震,震级从 -1.9 到 5.0 不等。基于地震位置、聚焦机制和震级的调查共同揭示了沿早期构造事件中已存在的断层分布的独特地震群。从该阵列中恢复的数据为和平河地区的构造历史和地震风险提供了独特而重要的制约因素。
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