Bodily tides provide key information on the interior structure, evolution, and origin of the
planetary bodies. Our Solar system harbors a very diverse population of planetary bodies …

A novel and comprehensive method is proposed for calculating the dislocation Love
numbers (DLNs), Green's functions (GFs), and the corresponding deformation in a …

The S-wave velocity (V s) structure of sediments and the uppermost crust in the landward
slope of a subduction zone are important for determining the dynamics of the overriding …

The Airy phase is the frequency at which group velocity of a surface acoustic wave (SAW)
attains a stationary value. In turn, a stationary value of the group velocity causes SAW to …

This study investigates the propagation of Stoneley waves at the interface between two semi-
infinite, size-dependent couple stress solids, taking into account imperfect interface …

Dispersion inversion of Scholte wave is an effective method for constructing the shear wave
velocity models of seabed sediments, but it is usually conducted based on the elastic …

The generation of microseisms is investigated at the ALOHA Cabled Observatory (ACO)
north of Oahu during the close passage of Hurricane Lester in September 2016. Sensors …

The underwater multichannel analysis of surface wave (UMASW) is becoming an essential
tool for surveying subbottom shear wave velocity. Current practice is limited to interpretation …

The propagating of quasi-Scholte waves in a hydroelastic system consisting of an
orthotropic plate and a compressible inviscid fluid layer were investigated. There are …

A theory of pseudo-Scholte wave propagating in a saturated porous medium loaded on its
interface by a viscous compressible liquid is described. The porous medium is simulated by …