Monitoring changes of seismic properties at depth can provide a first‐order insight into
Earth's dynamic evolution. Coda wave interferometry is the primary tool for this purpose. This …

We document the arrival of seismic energy in the core shadow zone up to large distances
beyond 150° more than 100 s prior to the core phases. Numerical simulations of the energy …

Constraints on crustal and uppermost mantle structure provide key information for
understanding the geodynamic processes that have shaped the geological expressions and …

We numerically solve the acoustic radiative transfer equation for seismic S‐waves via Monte
Carlo simulation. By assuming a von Kármán‐type random medium with anisotropic …

Abstract The Central Anatolian Plateau with its volcanic provinces represents a broad
transition zone between the compressional deformation in the east and the extensional …

Accurate estimates of the moment magnitude of earthquakes that physically measure the
earthquake source energy are crucial for improving our understanding of seismic hazard in …

To investigate the small-scale elastic structure of the subsurface at length scales below the
resolution limits of waveform tomography, envelopes of high-frequency scattered seismic …

A proper estimate of moment magnitude, which is a physical measure of the energy
released at an earthquake source, is essential for better seismic hazard assessments in …

Intrinsic absorption and scattering properties provide us with information about the physical
state and heterogeneity of the Earth's crust. These properties are usually obtained by …

We applied sensitivity kernels based on perturbation theory to map the crustal intrinsic and
scattering attenuation of S wave envelopes in the southern Aegean. The southern Aegean …