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Seismic imaging˸ strategies for visco-acoustic full waveform inversion

Abstract : Seismic attenuation is a useful physical parameter to describe and to image the properties of specific geological bodies, e.g., saturated rocks and gas clouds. Classical approaches consist of analyzing seismic spectrum amplitudes or spectrum distortions based on ray methods. Full waveform inversion is an alternative approach that takes into account the finite frequency aspect of seismic waves. In practice, both seismic velocities and attenuation have to be determined. It is known that the multi-parameter inversion suffers from cross-talks.This thesis focuses on retrieving velocity and attenuation. Attenuation dispersion leads to equivalent kinematic velocity models, as different combinations of velocity and attenuation have the same kinematic effects. I propose a hybrid inversion strategy: the kinematic relationship is a way to guide the non-linear full waveform inversion. The hybrid inversion strategy includes two steps. It first updates the kinematic velocity, and then retrieves the velocity and attenuation models for a fixed kinematic velocity. The different approaches are discussed through applications on 2D synthetic data sets, including the Midlle-East and Marmousi models.
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Submitted on : Thursday, October 10, 2019 - 10:35:15 AM
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  • HAL Id : tel-02310410, version 1


Hao Jiang. Seismic imaging˸ strategies for visco-acoustic full waveform inversion. Earth Sciences. Université Paris sciences et lettres, 2019. English. ⟨NNT : 2019PSLEM013⟩. ⟨tel-02310410⟩



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