S049-06
Local distance seismic source classification during the iMUSH project

Monday, 14 December 2020: 19:22
Virtual
Ruijia Wang, University of New Mexico Main Campus, Albuquerque, NM, United States, Brandon Schmandt, University of New Mexico, Department of Earth & Planetary Sciences, Albuquerque, NM, United States and Keith D. D Koper, University of Utah, Department of Geology and Geophysics, Salt Lake City, UT, United States
Abstract:
Explosions and earthquakes are effectively discriminated by P/S amplitude ratios for moderate magnitude events (M≥4) observed at regional to teleseismic distances (≥200 km). It is less clear if P/S ratios are effective explosion discriminants for lower magnitude events observed at shorter distances. We report new tests of P/S discrimination using a dense seismic array in a continental volcanic arc setting near Mount St. Helens, with 23 single-fired borehole explosions (ML 0.9–2.3) and 406 earthquakes (ML 1–3.3). The array provides up to 95 three-component broadband seismographs and most source-receiver distances are <120 km. Potential controls on local distance P/S ratios are investigated, including: frequency range, distance, magnitude, source depth, number of seismographs, and site effects. A frequency band of about 10–18 Hz performs better than lower or narrower bands because explosion-induced S-wave amplitudes diminish relative to P for higher frequencies. Source depth and magnitude exhibited weak influences on P/S ratios. Site responses for earthquakes and explosions are correlated with each other and with shallow crustal Vp and Vs from travel-time tomography. Overall, the results indicate high potential for local distance P/S explosion discrimination in a continental volcanic arc setting, with ≥98% true positives and ≤6.3% false positives when using the array median from ≥16 stations. Performance is reduced for smaller arrays, especially those with ≤4 stations, thereby emphasizing the importance of array data for discrimination of low magnitude explosions. When only a sparse network is available, preliminary tests show that combining P/S ratios with depth sensitive differential magnitudes, ML–MC, can improve source discrimination. Lastly, we analyze the focal mechanisms of explosions and earthquakes through both first motion polarity and full moment tensor inversion. Our integrated source study in such a structurally complex region shows promising results in local distance source discriminations.