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Products Technology | Why SeisOpt®? | Request References | Case Studies SeisOpt 2D
Download this brochure by clicking here.
Automatically predict 2-D velocity structure?
Use seismic in geologically complex areas?
Decrease field deployment costs?
Interactively & Automatically design seismic arrays
Make sure you have sampled your target
See velocity and sampling information
Batch process your data...
Decrease analysis costs and increase productivity?
![]() The power is under your fingertips!TM
![]() Figure 1. Run the optimization, visualize and analyze the velocity model and make final figures. Use the 'tuner' to further fine-tune the optimized velocity model and/or create new velocity models and use SeisOptŪ @2D as a bidding module
![]() Figure 2. Use the virtual survey design module to visualize and optimize subsurface ray coverage and your seismic array during data acquisition, thus saving both time and money. Know your target is sampled before leaving the field
![]() Figure 3. The SeisOptŪ @2D Graphical User Interface allows you to compare first-arrival travel time picks to theoretical travel times calculated through the velocity model, for each seismic source.
![]() Figure 4. Using MakeEPS, final figures can be saved in encapsulated PostScript format. This can then be imported into other popular programs for further editing or incorporation into report text. What is the Technology behind SeisOptŪ @2D? SeisOptŪ velocity optimization software achieves a globally optimized velocity model using only first arrival travel time data and array geometry as input. SeisOpt requires no prior assumptions of subsurface structure, or any other subjective data, as input. SeisOpt technology is now being used throughout the world for geotechnical, mining and petroleum applications. The technology is based on a nonlinear optimization method called generalized simulated annealing. The algorithm performs repeated forward modeling, where new models are conditionally accepted or rejected based on a probability criterion. This criterion allows the algorithm to escape from non-unique, local, travel-time minima to achieve a unique, globally optimized model of subsurface velocity structure. The algorithm makes no assumptions on the orientation of the subsurface velocity gradient, and can therefore reveal vertical structures and strong lateral gradients, if present. The method is therefore ideal in areas characterized by strong lateral velocity gradients, and in areas with extreme topography or complex near-surface structure where the user has little or no prior knowledge of subsurface structure.
If you want try SeisOptŪ @2D, contact us at
www.optimsoftware.com |
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