Surface-wave retrieval using Seismic Interferometry by multi-dimensional deconvolution

In this thesis, seismic interferometry by multi dimensional deconvolution is used to retrieve the surface-wave response from a virtual source to a receiver by using the observations due to, often passive, noise sources located elsewhere. The virtual source response is used to retrieve the phase velocity, a property used for shallow subsurface velocity models.Applied Geophysics and PetrophysicsGeoscience & EngineeringCivil Engineering and Geoscience