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High‐resolution 3‐D P wave attenuation structure of the New Madrid Seismic Zone using local earthquake tomography
Author(s) -
Bisrat Shishay T.,
DeShon Heather R.,
Pesicek Jeremy,
Thurber Clifford
Publication year - 2014
Publication title -
journal of geophysical research: solid earth
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.983
H-Index - 232
eISSN - 2169-9356
pISSN - 2169-9313
DOI - 10.1002/2013jb010555
Subject(s) - seismology , seismometer , geology , attenuation , crust , induced seismicity , amplitude , fault (geology) , seismic tomography , seismic wave , p wave , tomography , mantle (geology) , geophysics , physics , optics , medicine , cardiology , atrial fibrillation
A 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 ( M D < 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 Q P 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 Q P (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 Q P 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.