Oluwaseyifunmi Emmanuel Adeboboye , Lindsay Chuang, Miguel Neves, Zhigang Peng , Dan Frost, Steve Jaume

An unusual earthquake swarm began in December 2021 between the towns of Elgin and Lugoff in South Carolina, United States. This area is characterized by historically low seismicity, but by April 2024 it has experienced 97 small earthquakes listed in the USGS catalog, presenting a unique opportunity to investigate the dynamics of earthquake swarms in stable continental regions. These events are located in a north-south diffuse trend, cross-cutting the Eastern Piedmont Fault System (EPFS), a Late Paleozoic dextral strike-slip fault, however, the location uncertainties were too large to reveal any obvious structure. Starting from October 2022, we deployed 85 Smartsolo 5-Hz 3-component nodal stations for four months in the direct vicinity of the Elgin swarm. By using a combination of deep learning and match filter techniques (MFT) for event detection, and double-difference relocation methods for precise earthquake locations, we obtain up to 100 high-resolution microearthquake locations, as compared with 4 events listed in the USGS catalog for the deployment period. In our improved catalog, we report significantly smaller magnitudes in comparison to those listed in the USGS catalog, with a local magnitude ranging from -2.17 to 2.54 and achieving a magnitude of completeness at -0.22. The relocated catalog outlined a single fault plane of nearly north-south strike and west-dipping, generally consistent with one of the magnetic anomalies in this region (Shah et al., 2023). We also determine focal mechanisms solutions for selected events in this swarm sequence which shows mainly strike-slip faulting with nodal planes aligning with the north-south striking seismic cluster. Our relocated catalog can be used to constrain the location of other swarm events outside the nodal recording period and provide a robust benchmark dataset for further analysis of the swarm sequence.