Least-Squares Reverse Time Migration with Threshold Shrinkage
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Solution Overview
Problem
Migration algorithms for seismic data inversion are computationally intensive and struggle with blurring due to random noise and migration artifacts, leading to slow convergence and low-resolution images, especially in complex subsurface geologies.
Innovation Solution
The implementation of a least-squares reverse time migration method using an adjoint migration operator and a threshold shrinkage function, which includes a sign function and a maximum function, to update the property model and improve image resolution by attenuating noise and artifacts.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Measurement precision
If migration algorithms are used to convert time-based seismic data into depth representation, then subsurface imaging is achieved, but computational cost and processing time increase significantly
Solution Approach 1:
The patent applies least-squares optimization to update the property model iteratively, changing the mathematical approach from conventional migration to a physics-based inversion framework. This transforms the problem parameters and convergence characteristics, achieving higher resolution while managing computational load through efficient update schemes
Solution Approach 2:
The patent segments the seismic inversion process into distinct stages: initial property model creation, iterative least-squares updates using conjugate gradient solver, and threshold shrinkage refinement. This segmentation allows each stage to be optimized independently, reducing overall computational time while maintaining image quality
2Reliability
If conventional migration algorithms are used, then subsurface imaging is performed, but image quality deteriorates due to blurring from random noise and migration artifacts
Solution Approach 1:
The patent converts the harmful effects of noise and artifacts by using the threshold shrinkage function to identify and attenuate these features. The least-squares inversion framework transforms random noise into structured updates that can be systematically reduced, converting what was previously harmful into a controllable aspect of the inversion process
Solution Approach 2:
The patent introduces an intermediate property model that acts as a mediator between the raw seismic data and the final migrated image. This property model undergoes iterative refinement through least-squares updates and threshold shrinkage, serving as an intermediary that filters out noise and artifacts while preserving genuine subsurface features
3Measurement precision
If complete migration-wavefield inversion is performed, then accurate subsurface representation is achieved, but the number of iterations required increases computational intensity
Solution Approach 1:
The patent applies partial action by performing least-squares updates only on the property model rather than complete wavefield inversion at each step. The conjugate gradient solver is used iteratively with a limited number of inner iterations, providing sufficient accuracy without the full computational burden of complete inversion at every outer iteration step
Solution Approach 2:
The patent performs preliminary action by first creating an initial property model using conventional migration, then using this as the starting point for least-squares refinement. This preliminary model provides a reasonable initial guess that reduces the number of iterative updates needed to achieve convergence, improving overall processing efficiency
Data Source
AI summary
A method may include obtaining seismic data regarding a geological region of interest. The method may further include obtaining a property model regarding the geological region of interest. The method may further include determining an adjoint migration operator based on the property model. The method may further include updating the property model using the seismic data and a conjugate gradient solver in a least-squares reverse time migration to produce a first updated property model. The conjugate gradient solver is based on the adjoint migration operator. The method may further include updating the first updated property model using a threshold shrinkage function to produce a second updated property model. The threshold shrinkage function comprises a sign function and a maximum function that are applied to the first updated property model. The method may further include generating a seismic image of the geological region of interest using the second updated property model.


