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Adewale Amosu (Wale) Center for Earthquake Research and Information University of Memphis Joint Inversion of Receiver Functions and Surface Wave Dispersion for New Madrid Seismic Zone.
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Adewale Amosu (Wale)Center for Earthquake Research and InformationUniversity of MemphisJoint Inversion of Receiver Functions and Surface Wave Dispersion for New Madrid Seismic Zone
Iuse the Computer Programs in Seismology codes (Hermann & Ammon, 2002).The joint inversion aims to find a 1D model for Surfacewave velocity The model aims to minimize the following NRF and Ns are Receiver Function and Rayliegh Wave Phase Velocity Data Data, O=observed, P=predicted Ρ and λ control how much influence each data set has Topographic map showing earthquakes greater than magnitude 2.5 (circles) of the central United States. Source: USGS I hope to obtain better estimates of Moho depth and Velocities in the Region