Ground response analyses (GRA) model the vertical propagations of SH waves through flat-
layered media (1DSH) and are widely carried out to evaluate local site effects in practice …

The incorporation of local amplification factors (AFs) determined through site response
analyses has become standard practice in site-specific probabilistic seismic hazard analysis …

A significant amount of seismic site response research over the past decade has focused on
our abilities to replicate recorded ground motions at borehole array sites, where both the …

One-dimensional site response analyses (1D SRAs) with shear-wave velocity (VS)
randomization are commonly performed to estimate median site-specific amplification …

Earthquake-induced ground motions are determined by a combination of source, path, and
site effects. As seismic waves propagate along a path from the fault rupture to a given site …

The Atlantic and Gulf Coastal Plains (CPs) are characterized by widespread accumulations
of low-velocity sediments and sedimentary rock that overlay high-velocity bedrock. Geology …

One-dimensional site response analysis (1D SRA) remains the state of practice to estimate
site-specific seismic response, despite the ample evidence of discrepancies between …

The orientation variability of earthquake ground motions (ie, GM directionality) is an
important engineering characteristic in the seismic design of structures. The GM …

One‐dimensional site response analysis (1D SRA) remains the standard practice in
considering the effect of local soil deposits and predicting site‐specific ground motions …

In this study, the one-dimensional nonlinear Matasovic model was extended to the two-and
three-dimensional stress space by replacing the shear strain with the generalized shear …