--> Geological Interpretation Using Pattern Recognition from Self-Organizing Maps and Principal Component Analysis
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Geological Interpretation Using Pattern Recognition from Self-Organizing Maps and Principal Component Analysis

Abstract

Since the late 1970s, the explosion of various kinds of Previous HitseismicNext Hit Previous HitattributesNext Hit derived from the acquired Previous HitseismicNext Hit signal has been the boon and the bane of the interpreter. Now the interpretation of reflection data requires powerful computers and advanced visualization software packages, but the interpreter is always looking for ways of distilling vast amounts of data down to essential volumes necessary to make prudent choices for reducing risk in picking drilling locations.

Previous HitSeismicNext Hit Previous HitattributesNext Hit are considered to be any measurable properties of the Previous HitseismicNext Hit signal. They can be measured at one instance in time or depth, or in a window of time or depth. They can be single trace measurements, multiple traces, or even on a surface interpreted in the data. Common categories of Previous HitseismicNext Hit Previous HitattributesNext Hit include the instantaneous (e.g., frequency, phase, Q), geometric (e.g., coherence, curvature), amplitude enhancing (e.g., sweetness, relative acoustic impedance, average energy), amplitude variations with offset (AVO) (e.g., fluid factor, intercept, gradient), spectral decomposition (e.g., either envelope based or wavelet based) and inversion (e.g., Poisson's ratio, density, brittleness, and more).

The use of principal component analysis (PCA), which is a linear quantitative process designed to understand which Previous HitseismicNext Hit Previous HitattributesNext Hit have interpretative significance by analyzing the variations in the data, has proven to be an excellent approach to sorting through vast amounts of data. PCA used in the interpretation workflow can help determine meaningful Previous HitseismicNext Hit Previous HitattributesNext Hit, and in turn, these Previous HitattributesNext Hit can be used as input into neural analysis in the creation of self-organized maps (SOM). SOM analysis is a pattern recognition process using unsupervised neural networks, and can reveal the natural clustering and patters in the data which often are distinct geological features not easily identifiable using singular Previous HitseismicNext Hit Previous HitattributesTop.

Several case histories using PCA and SOM, in both conventional and unconventional reservoirs, will be reviewed to show the importance of these time-saving tools when added to the interpretation workflow.