A unique, stable and mature combination of production and interactive seismic data processing

3D Grid-based Tomography

Update subsurface velocity and anisotropic material parameters along a predefined coarse grid.

Paradigm® GeoDepth® Tomography supports both grid-based and model-based methods that can be used according to the problem to be solved. For example, Gulf of Mexico sediments affected by long period compaction are normally parameterized by a Cartesian grid.

Velocity volume updates

3D grid tomography updates velocity volumes and (optionally) volumes of the anisotropic parameters ε and δ. The updates are calculated on a spatial grid which is generally coarser than the velocity volume. The updates can be constrained to honor the structure. After calculations are completed, the updates are interpolated to the size of velocity and anisotropic parameter grids. The interpolated updates are added to the current volumes to produce new volumes of velocities and anisotropic parameters, again taking into account the geological structure.

3D grid tomography can use well markers in the form of mistie maps as an additional constraint on the updated subsurface model.

Paradigm grid-based tomography supports Ocean Bottom Cable acquisitions.

Integrating VSP data reduces uncertainty in the model building process, resulting in fewer iterations and quicker delivery of the final model.

Incorporating VSP data into the tomographic inversion process can yield very accurate results, especially when updating anisotropic parameters.  The information in VSP seismic data is superior to that of reflection seismic data, as it avoids the ambiguity of depth vs. velocity. Grid-based Tomography now supports first arrival VSP data, which can be used alone or together with regular reflection seismic data (CIG's).  Grid-based Tomography uses point-to-point ray tracing to converge from the receivers in the borehole to the surface acquisition. 

Well tie tomography

Tying the horizons interpreted on the seismic image to well markers plays a critical role in the velocity model building workflow, especially in the presence of anisotropy. The aim is to find a velocity model that yields flat gathers after depth migration, and ties to the well markers. Subsurface velocities cannot be uniquely determined by the surface recorded seismic data alone; in such cases, it’s possible to find a velocity that will flatten the gathers but not tie to the wells.  Well information is used to reduce this ambiguity and generate a geologically plausible velocity model.

Mis-ties between seismic horizons and well markers are calculated and used as input to well tie tomography to update the velocity/anisotropic parameters, resulting in a velocity model that minimizes the input mis-ties.

Direct 3D grid-based tomography

For large-scale models and especially those with high-resolution update grids, where the size of the tomography matrix can be too large (quadratic with the number of model parameters) to be handled even by the largest super-computers, a new approach is required. GeoDepth 3D direct grid-based tomography has have been shown to overcome these inherent limitations by reducing the memory and disk space required through more intense computation.

While the resulting updated subsurface velocities are identical to those of conventional 3D grid tomography, the difference is in the implementation. In 3D direct tomography, the tomography matrix is never generated explicitly, dramatically reducing the memory and disk space required by the application, where the inversion process (including ray tracing and the construction of the tomography equations) is performed in a single stage using an iterative process.

Direct tomography implementation advantage:

  • Can handle large 3D updated grids (either due to the size of the survey or due to the requirements for high resolution) that could not be used before.
  • Is very efficient when using clusters with massive amounts of nodes.

The runtime of direct tomography is mainly related to CPU power in globally running the ray tracing many times (for each iteration), whereas conventional 3D grid-based tomography suffers mainly from being I/O bounded, where most of the time is spent reading and manipulating the tomography matrix (many terabytes of data).