Our models and understanding of the dynamics of earthquake rupture are based largely on
estimates of earthquake source parameters, such as stress drop and radiated seismic …

We develop a generic ground‐motion prediction equation (GMPE) that can be adjusted for
use in any region by modifying a few key model parameters. The basis of the GMPE is an …

Empirical ground‐motion prediction equations (GMPE s) require adjustment to make them
appropriate for site‐specific scenarios. However, the process of making such adjustments …

In this study we derive a spectral model describing the source, propagation and site
characteristics of S waves recorded in central Italy. To this end, we compile and analyse a …

We modeled the source and attenuation attributes of well‐recorded M 6+ earthquakes
based on the equivalent point‐source approach, with the goal of determining how to treat …

We develop an empirical model of the decay of Fourier amplitudes for earthquakes of M 3–6
recorded on rock sites in eastern North America and discuss its implications for source …

Response spectra for California earthquakes of 3.0≤ M< 7.5 are well described by a simple
stochastic ground‐motion model using an equivalent point‐source concept. We determine …

We update ground‐motion prediction equations (GMPE s) for eastern North America (ENA)
using the referenced empirical approach of. The technique is based on the use of residual …

Local geologic structure and topography may modify arriving seismic waves. This inherent
variation in shaking, or “site response,” may affect the distribution of slope failures and …

To better characterize seismic hazard, particularly, for induced seismicity, there is an
increasing interest in methods to estimate moment magnitude (⁠ M w⁠) for small …