High‐resolution 3‐D P wave attenuation structure of the New Madrid Seismic Zone using local earthquake tomography

Abstract

AbstractA three‐dimensional (3‐D), high‐resolution P wave seismic attenuation model for the New Madrid Seismic Zone (NMSZ) is determined using P wave path attenuation (t*) values of small‐magnitude earthquakes (MD < 3.9). Events were recorded at 89 broadband and short‐period seismometers of the Cooperative New Madrid Seismic Zone Network and 40 short‐period seismometers of the Portable Array for Numerical Data Acquisition experiment. The amplitude spectra of all the earthquakes are simultaneously inverted for source, path (t*), and site parameters. The t* values are inverted for QP using local earthquake tomography methods and a known 3‐D P wave velocity model for the region. The four major seismicity arms of the NMSZ exhibit reduced QP (higher attenuation) than the surrounding crust. The highest attenuation anomalies coincide with areas of previously reported high swarm activity attributed to fluid‐rich fractures along the southeast extension of the Reelfoot fault. The QP results are consistent with previous attenuation studies in the region, which showed that active fault zones and fractured crust in the NMSZ are highly attenuating.