Full-waveform inversion of seismic data using instantaneous-phase coherency

Full-waveform inversion of seismic data using instantaneous-phase coherency

Schaly, Jan (TU Delft Civil Engineering & Geosciences)

Draganov, D.S. (mentor)
Staring, M. (mentor)
Weemstra, C. (graduation committee)
Wellmann, F. (graduation committee)

Delft University of Technology
ETH Zürich
RWTH Aachen University

Delft University of Technology
ETH Zürich
RWTH Aachen University

Applied Geophysics | IDEA League

2022-08-26

With a rapid increase in computational resources two dimensional full-waveform inversion is evolving into a promising tool for near-surface geophysics. However, near-surface applications suffer from local minima due to amplitude errors associated with two dimensional full-waveform inversion. By clever definition of the misfit function, the influence of the amplitude errors can be mitigated. Here, I use a recently proposed misfit function based on the instantaneous-phase coherency. The instantaneous-phase coherency misfit function uses complex trace analysis to create an amplitude unbiased misfit function. First, I compare the new misfit function to a traditional least-squares misfit function by inverting synthetic models where noise is added, a field dataset containing Rayleigh waves and a field dataset containing Love waves. Next, I perform inversions on layer cake models to investigate the accuracy of the full-waveform inversion using the new misfit function and finally, I test the robustness of the inversion by using a complex subsurface model. The inversions performed on the synthetic models show that the instantaneous-phase coherency misfit is more robust when noise is introduced to the data compared to the least-squares misfit. Furthermore the two field datasets, demonstrate the ability of the instantaneous-phase to deliver accurate near-surface results when used on field data. The results from the layer cake inversions where inconclusive, however I did demonstrate that a better selection of the bandwidth did improve the result. Finally, the results from the complex subsurface model show that the instantaneous-phase coherency is able to resolve parts of the complex subsurface model.

Full-waveform inversion
Instantaneous-phase coherency
Inversion
Seismic
Finite Difference

http://resolver.tudelft.nl/uuid:4f041ee4-2253-45c8-8042-3d621e836d89

2023-06-01

Student theses

master thesis

© 2022 Jan Schaly