Other than the Crittenden County fault zone (CCFZ), little is known about the seismic hazard from faults within 50 km of Memphis, Tennessee, a city that contains a large inventory of older buildings that are vulnerable to moderate and strong earthquake ground shaking. To address this lack of knowledge, reconnaissance high-resolution seismic-reflection surveys using Mini-Sosie (Williams et al. 2001) and both P- and S-wave hammer sources (this study) were acquired at the boundary between the loess-covered bluffs (upland area) and the modern Mississippi River floodplain in Meeman-Shelby Forest State Park about 25 km north of Memphis...
You do not have access to this content, please speak to your institutional administrator if you feel you should have access.
