Q estimation and compensation for attenuated seismic data with the scanning-Q nonstationary sparse inversion method
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DOI: 10.1190/geo2024-0746.1
Abstract: Influenced by the absorption and attenuation of wave propagation media, seismic waves experience amplitude attenuation, frequency reduction, and phase distortion. This absorption-attenuation is directly linked with the viscoelastic properties and can be quantified by the… read more here.
Keywords: shallow deep; method; scanning nonstationary; seismic data ... See more keywords