Lithospheric structure of the central Andes based on surface wave dispersion

Using the isotropic component of the phase velocity maps to constrain regional variations in shear velocity and Moho-depth, we observe that over the upper-middle crust depth range

(1) has been used to set up tomographic inverse problems, based upon the ray theory approximation, to derive global maps of the azimuthal anisotropy of Rayleigh and Love waves

CHARACTERIZATION OF FRENCH ACCELEROMETRIC PERMANENT NETWORK STATIONS WITH SURFACE-WAVE BASED METHODS: IMPORTANCE OF JOINT USE OF ACTIVE AND PASSIVE METHODS, LOVE AND RAYLEIGH

The power spectrum, the nonlinear dispersion relation and the PDF of the Fourier modes show strong effects of non- linear waves involved in wave turbulence. This suggests that

A linear approximation of the Rayleigh wave phase velocity is used to associate the phase velocity variations with the model variations, by using the sensitivity kernel (i.e.

A joint inversion of Rayleigh wave velocities and receiver functions (Dugda et al., 2007) and a previous S-to-P receiver function study (Rychert et al., 2012) imaged the shear

We model the fundamental mode Rayleigh wave together with its first four overtones, thereby increasing our sensitivity to the shear wave velocity structure at the base of the

Paleogene clockwise tectonic rotations in the forearc of central Andes, Antofagasta region, northern Chile... Paleogene clockwise tectonic rotations in the forearc of central