Hi,

does anyone know if secondary Love waves can be generated by Rayleigh wave interaction with a sedimentary basin boundary?

I have found prior work that showcases generation of secondary Rayleigh and Love waves due to the incident of S-waves on sedimentary basin boundaries for both the observational case and numerical calculations. From a purely simplified point of view the horizontal energy of a Rayleigh wave should excite Love waves when hitting a perpendicular sedimentary boundary.

Does anyone know of any results pointing towards or against such mechanism.

Any help is greatly appreciated.

More Martin Gal's questions See All
Similar questions and discussions