Seismic Dip Decimation for Efficient, Accurate RGT Image Computation
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Solution Overview
Problem
Seismic images have large dimensions and significant data volumes, which can take a long time to process, especially with iterative schemes like [LOMASK2006], and may not be compatible with existing graphical processing units, impacting the accuracy of chrono-stratigraphic analysis.
Innovation Solution
A method involving decimating the seismic dip image by a factor along horizontal dimensions, initializing decimated seismic horizon surfaces, and iteratively modifying them to align with local seismic dips, while maintaining vertical resolution for accurate RGT image computation.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Measurement precision
If iterative schemes like LOMASK2006 are used to process seismic images, then accuracy of RGT image computation is improved, but processing time increases significantly
Solution Approach 1:
The patent applies segmentation by dividing the seismic image processing into two distinct stages: (1) computing seismic dips at full resolution to capture accurate local gradient information, and (2) processing the decimated image with iterative schemes to reduce computational burden. This segmentation allows the computationally intensive iterative processing to operate on reduced data while still achieving accurate RGT images through the guidance of full-resolution dip information.
Solution Approach 2:
The patent implements preliminary action by computing the seismic dip image at full resolution before decimation. This preliminary computation of local gradient information provides a foundation that guides the subsequent iterative processing on decimated data, ensuring that even though the iterative scheme operates on reduced-resolution data, it benefits from the accurate dip constraints established in advance.
2Measurement precision
If full-resolution seismic images are processed, then accuracy of chrono-stratigraphic analysis is improved, but data processing volume becomes unmanageable for existing GPUs
Solution Approach 1:
The patent extracts the most critical information from the full-resolution seismic image by computing the seismic dip image, which captures the local gradient information necessary for accurate horizon picking. This extracted dip information is then used to guide the iterative processing on decimated data, allowing the system to work with reduced data volumes while maintaining accuracy through the extracted gradient constraints.
Solution Approach 2:
The processing is segmented into full-resolution dip computation followed by decimated iterative processing. This segmentation allows the system to retain full-resolution information where it matters most (in the dip constraints) while using reduced-resolution data for the computationally intensive iterative horizon picking, thereby managing data volume for existing GPUs.
3Productivity
If decimation is applied to reduce data volume, then processing efficiency is improved, but resolution and accuracy may be degraded
Solution Approach 1:
The patent applies local quality by computing seismic dips at full resolution to preserve local gradient information accuracy, while allowing decimation in regions where full resolution is less critical for the iterative horizon picking process. This ensures that local accuracy is maintained where it matters most (in the dip constraints) while achieving overall processing efficiency through selective decimation.
Data Source
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AI summary
The present disclosure relates to a computer implemented method (30) for processing a seismic image comprising at least one horizontal dimension and one vertical dimension, said method comprising: - (S30) determining a seismic dip image based on the seismic image; - (S31 ) decimating the seismic dip image by a decimating factor along at least one horizontal dimension in order to obtain a decimated seismic dip image; - (S32) initializing decimated seismic horizon surfaces; - (S33) iteratively modifying the decimated seismic horizon surfaces to progressively increase alignment between local orientations of each decimated seismic horizon surface and the corresponding local seismic dips of the decimated seismic dip image, said local orientations or local seismic dips being corrected by the decimating factor, until a predetermined stop criterion is satisfied; - (S35) determining a relative geological time, RGT, image based on the decimated seismic horizon surfaces.