Seismic ray theory Page 1 Seismic ray theory Vlastislav Cervený 1) and Ivan Pšencık 2) 1)
Charles University, Faculty of Mathematics and Physics, Department of Geophysics, Prague …

The Northridge earthquake caused 1.78 g acceleration in the east-west direction at a site in
Tarzana, California, located about 6 km south of the mainshock epicenter. The …

We discuss the subsurface structure of the Karadere–Duzce branch of the North Anatolian
Fault based on analysis of a large seismic data set recorded by a local PASSCAL network in …

We present a technique to infer the rupture history of an earthquake from near‐source
records of ground motion. Unlike most previous studies, each point on the fault is assumed …

We analyze temporal variations of seismic velocity along the Karadere-Düzce branch of the
north Anatolian fault using seismograms generated by repeating earthquake clusters in the …

Dynamic-crack earthquake simulations generally assume that the crustal material
surrounding faults is laterally homogeneous. Tomographic and near-fault seismic studies …

Numerical modelling of high-frequency seismic wave fields in complex, 2-D and 3-D,
laterally varying, layered structures by the summation of elastodynamic Gaussian beams is …

Two instances of fault zone trapped seismic waves have been observed. At an active normal
fault in crystalline rock near Oroville in northern California, trapped waves were excited with …

Near-source strong motion velocity records and teleseismic short-period P waveforms are
modeled to obtain the spatial and temporal distribution of slip for the 1984 Morgan Hill …

A two‐dimensional solution for the scalar wave equation in a model of two vertical layers
between two quarter spaces is used to study properties of seismic waves in a laterally …