Orthogonal Function Estimation for AVOA Seismic Data Resolution

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Solution Overview

Problem

Current seismic data processing methods are inadequate for precise Amplitude Variation with Offset (AVO) and Amplitude Variation with Offset and Azimuth (AVOA) characterization, as they require small azimuth sectors for resolution, leading to under-sampling and reduced processing efficiency, and fail to correlate AVO variations between sectors.

Innovation Solution

A method that organizes seismic traces according to acquisition parameters, defines a base of orthogonal elementary functions, and determines combination coefficients to estimate amplitude variations, allowing for precise AVOA characterization across all data without sector separation, preserving azimuth resolution and enabling multi-dimensional AVOA characterization.

Engineering Contradictions & Design Principles

VSEngineering Contradiction Analysis

1Measurement precision

If seismic data is separated into multiple azimuth sectors for AVO characterization, then the resolution of AVOA characterization is improved, but the number of traces in each subset is reduced leading to under-sampling and reduced processing efficiency

Engineering Contradiction:
ImproveAVOA characterization resolutionVSAvoidprocessing efficiency
Core Design Contradiction:
Measurement precisionVSProductivity

Solution Approach 1:

The patent applies segmentation by dividing the azimuth range into multiple sectors (e.g., 0-45°, 45-90°, etc.), allowing AVOA characterization to be performed separately in each sector. This segmentation enables precise measurement of azimuthal variations while maintaining sufficient trace counts within each sector for reliable statistical analysis and processing efficiency.

Inventive Principle:
Principle #1Segmentation

2Measurement precision

If the aperture angle of azimuth sectors is reduced to maintain AVO characterization resolution, then the measurement precision is improved, but the number of traces in each subset is reduced causing under-sampling

Engineering Contradiction:
ImproveAVO characterization resolutionVSAvoidnumber of traces
Core Design Contradiction:
Measurement precisionVSQuantity of substance

Solution Approach 1:

The patent transitions from traditional 2D AVO analysis to 3D AVOA analysis by incorporating the azimuth dimension. This dimensional expansion allows the use of multiple azimuth sectors simultaneously, where each sector maintains sufficient trace coverage while collectively providing comprehensive azimuthal coverage. The method effectively utilizes the additional azimuth dimension to resolve the trade-off between sector aperture and trace density.

Inventive Principle:
Principle #17Another dimension (Dimensionality change)

3Ease of operation

If traditional AVO methods are used that assume linear amplitude variation, then the processing simplicity is maintained, but the accuracy of AVOA characterization is degraded

Engineering Contradiction:
Improveprocessing simplicityVSAvoidAVOA characterization accuracy
Core Design Contradiction:
Ease of operationVSMeasurement precision

Solution Approach 1:

The patent changes the functional form of amplitude variation from the traditional linear model to a quadratic model that includes azimuthal dependence. The new model incorporates additional parameters (azimuthal coefficients) that capture the complex amplitude variations more accurately. This parameter expansion maintains processing systematicity while significantly improving AVOA characterization accuracy by accounting for non-linear effects.

Inventive Principle:
Principle #35Parameter changes

Data Source

PatentUS7369944B2Method of processing seismic data for AVO or AVOA characterization
Publication Date: 2008.05.06 CGGVERITAS SERVICES
  • US7369944B2 patent drawing
  • US7369944B2 patent drawing
  • US7369944B2 patent drawing

AI summary

The invention relates to a method of processing seismic data comprising a gather of seismic traces organised according to one or several acquisition parameters, each trace comprising a seismic signal defined by an amplitude as a function of time or depth, the method comprising the steps of:a) defining a base of elementary functions of the acquisition parameter(s),b) orthogonalising said elementary functions so as to define a base of orthogonal elementary functionsc) for a given time or at a given depth, determining combination coefficients defining a combination of the orthogonal elementary functions, said combination being an estimator of a variation in the amplitude of the seismic signal as a function of the acquisition parameter(s).