Surface-wave retrieval using Seismic Interferometry by multi-dimensional deconvolution
More Info
expand_more
expand_more
Abstract
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.
Files
Surface-wave_retrieval_using_S... (pdf)
(pdf | 2.38 Mb)