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Technical Content
Quantitative inversion of azimuthal anisotropy parameters from isotropic techniques
Quantitative inversion of azimuthal anisotropy parameters from isotropic techniques
A new method is outlined that allows you to use isotropic seismic modeling and inversion technology in an anisotropic setting. The method is based on the mapping of the isotropic elastic parameters into effective elastic parameters, appropriate for the expected type of anisotropy. This ...
Unlocking the tectonic history offshore Southern Gabon with high resolution seismic, gravity and magnetics
Unlocking the tectonic history offshore Southern Gabon with high resolution seismic, gravity and magnetics
A recent 3D Broadseis survey was performed in the southern offshore area of Gabon, showing a wealth of detailed information in the seismic data. Understanding how these structures relate to the tectonic evolution of this basin requires the integration of the concurrently acquired gravity ...
Data-driven interferometry method to remove spatially aliased and non-linear surface waves
Data-driven interferometry method to remove spatially aliased and non-linear surface waves
We propose a data-driven interferometry technique to remove low frequency aliased and non-conical surface waves in cross-spread domain. Despite insufficient sampling of the constructive regions in the cross-spread domain, the proposed approach has been designed for effectively handling any kind of 3D sparse geometry ...
Extending the reach of FWI with reflection data: Potential and challenges
Extending the reach of FWI with reflection data: Potential and challenges
We present a Reflection FWI (RFWI) workflow to update the velocity model using the low-wavenumber component of the FWI gradient of reflection data. This is achieved by alternately using high-wavenumber and low-wavenumber components to update density and velocity models, respectively. With synthetic examples, we ...
Applications of single-iteration Kirchhoff least-squares migration
Applications of single-iteration Kirchhoff least-squares migration
Least-squares depth migration approximates the inverse of the forward modeling. We show two real data applications of a single iteration (non-iterative) Kirchhoff least-squares depth migration process, generically referred to as migration deconvolution, to highlight the benefits of this process. Our first example demonstrates improved ...
Velocity model building challenges and solutions for seabed- and paleo-canyons: a case study in Campos Basin, Brazil
Velocity model building challenges and solutions for seabed- and paleo-canyons: a case study in Campos Basin, Brazil
The Campos Basin, offshore Brazil, features complex shallow geology in the forms of pronounced seabed canyons and paleo-canyons. The rapid variations in the velocity field due to these complex shallow geologic features can be difficult for ray-based tomography techniques to resolve, resulting in distorted ...
A 3-stage approach to derive key elastic properties for marine reservoir with faulted overburden
A 3-stage approach to derive key elastic properties for marine reservoir with faulted overburden
Seismic inversion transforms seismic reflection data into quantitative rock-property descriptions of a reservoir. Seismic data bandwidth is limited by signal-to-noise ratio, absorption, source wavelet, and shot and receiver ghosts. A typical deterministic seismic inversion workflow fills the low frequencies by extrapolating or interpolating existing ...
Improved iterative least-squares migration using curvelet-domain Hessian filters
Improved iterative least-squares migration using curvelet-domain Hessian filters
Least-squares migration (LSM) can potentially provide better amplitude fidelity, higher image resolution, and fewer migration artifacts than standard migration. Conventional LSM is often solved iteratively through linearized inversion, and therefore is often referred to as iterative LSM. In recent years, various single-iteration LSM approaches ...