Seismic Bedform Analysis for Lithology Estimation
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Solution Overview
Problem
Current methods for ascertaining lithology, connectivity, and porosity characteristics of subterranean formations are time-consuming and expensive, particularly in deep-water environments, requiring extensive core sample analysis.
Innovation Solution
The use of seismic data to analyze structural characteristics of bedforms, such as wavelength, wave height, bedform slope, asymmetry, and migration, to estimate grain size and subsequently infer lithology, connectivity, and porosity, thereby reducing the need for core samples.
Engineering Contradictions & Design Principles
Engineering Contradiction Analysis
1Measurement precision
If core sample analysis is used to determine lithology characteristics, then measurement precision is improved, but loss of time and cost increase significantly
Solution Approach 1:
The patent replaces the mechanical/physical core sampling and laboratory analysis system with a seismic data processing system. Seismic waves propagate through the subsformation and reflect off bedforms, allowing non-invasive measurement of lithology characteristics through computational analysis of seismic attributes rather than physical core extraction and lab testing
Solution Approach 2:
The patent introduces seismic data as an intermediary between the subsurface formation and the analyst. Instead of directly examining core samples, the system uses seismic reflections and processed attributes (such as amplitude, frequency, and waveform characteristics) as intermediaries to infer lithology properties indirectly through established geological relationships between bedform characteristics and lithology
2Measurement precision
If core sample analysis is used to determine lithology characteristics, then measurement precision is improved, but cost increases significantly
Solution Approach 1:
The patent replaces expensive core sampling operations, logistics, and laboratory analysis infrastructure with computational seismic data processing. The seismic data processing system uses algorithms to extract lithology information from existing seismic surveys, eliminating the need for costly core acquisition, transportation, and laboratory facilities
Solution Approach 2:
The patent creates a virtual model of the subsurface formation using seismic data processing. Instead of physically obtaining and analyzing core samples, the system generates a digital representation (copy) of the formation's lithology characteristics through seismic attribute analysis, allowing repeated analysis without additional physical sampling costs
3Productivity
If seismic data processing is used to estimate lithology, then productivity is improved, but measurement precision may decrease
Solution Approach 1:
The patent performs preliminary processing of seismic data to enhance the quality and interpretability of seismic attributes before lithology estimation. This includes noise filtering, signal enhancement, and calculation of derived attributes (such as instantaneous frequency, amplitude envelope, and curvature) that prepare the data for more accurate lithology prediction while maintaining computational efficiency
Solution Approach 2:
The patent incorporates feedback mechanisms where the results of lithology estimation are used to refine the seismic data processing parameters and models. By comparing predicted lithology with available well log data or core samples where available, the system iteratively improves the accuracy of the processing algorithms and attribute selection for better generalization to unseen formations
Data Source
AI summary
Methods for assessing lithology characteristics of bedforms within or relating to a subterranean formation using seismic data may include: assigning a bedform type to a bedform; extracting a cross-section of seismic data along the bedform in-line +/−15° with a fluid flow direction associated with the bedform; analyzing the cross-section to ascertain a structural characteristic of the bedform, wherein the structural characteristic comprises one or more of: a wavelength, a wave height, a bedform slope, a bedform asymmetry, a bedform migration, and a planform crest shape; and estimating a lithology for the bedform based on a correlation between (a) the lithology and (b) the bedform type and the structural characteristic.


