2013Research Repository (Delft University of Technology)Open access

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

V.M. De Waard

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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.

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What this paper is about

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.

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Available 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.

Key concepts: Seismic interferometry, Deconvolution, Interferometry, Geology, Blind deconvolution, Remote sensing, Passive seismic, Noise (video)

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