Imaging and characterizing shallow sedimentary strata using teleseismic arrivals recorded on linear arrays: An example from the Atlantic Coastal Plain of the southeastern U.S.

Thomas L Pratt, U.S. Geological Survey, Geologic Hazards Science Center, Reston, United States
Back to: Understanding the Influence of Near-Surface Materials on Seismic Wave Amplitudes: Methods for Measuring, Modeling, and Using Site Response I