Detecting Stratigraphic Features via Cross-Plotting of Seismic Discontinuity Attributes and Their Volume Visualization
Bibliographic record
Abstract
Fold and fault geometries, stratal architecture and large-scale depositional elements (e.g. channels,<br>incised valley-fill and turbidite fan complexes) are often difficult to see clearly on vertical and<br>horizontal slices through the seismic reflection data. Consequently, visualization techniques are used<br>for viewing the data, whether it’s the input seismic data or derived data in terms of seismic attributes.<br>Such visualization helps extract meaningful information, allows for greater interpretation accuracy and<br>improves efficiency. 3D volume rendering is one form of visualization that involves opacity control to<br>view the features of interest ‘inside’ the 3D volume. A judicious choice of opacity applied to edgesensitive<br>attribute sub-volumes such as curvature or coherence co-rendered with the seismic amplitude<br>volume can both accelerate and lend confidence to the interpretation of complex structure and stratigraphy.<br>In addition to co-rendering, we evaluate an interpretation workflow that cross-plots pairs of edgesensitive<br>attributes. By crossploting coherence and an appropriate curvature attribute, we can define a<br>polygon that highlights “clusters” that exhibit low coherence (indicating a discontinuity) and high<br>curvature (indicating folding, flexing, fault drag, or differential compaction). Modern volume<br>interpretation software allows us to link and display these interpreter-defined clusters in the seismic<br>volume for further examination. Once identified interactively, such visual ‘clustering’ can be used to<br>supervise geobody delineation using neural networks and other classification algorithms. This saves the<br>seismic interpreters considerable time and effort. We illustrate this new workflow through application<br>to several 3D seismic surveys recently acquired in western Canada and demonstrate that multiattribute<br>volume co-rendering and clustering provides a powerful tool that leads to a better understanding of the<br>spatial relationships between seismic attributes and the geologic objectives being pursued.
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How this classification was reachedexpand
Full frame distilled prediction
Teacher imitationNot calibrated prevalence, not ground truth. Human validation pending. Learned from the 10,348 direct Codex labels and 10,348 direct Gemma labels. Candidate is the union of thresholded teacher heads; consensus is their intersection. These outputs are machine_predicted_unvalidated and are not human labels or direct frontier model labels.
Codex and Gemma teacher scores by category
| Category | Codex | Gemma |
|---|---|---|
| Metaresearch | 0.000 | 0.000 |
| Meta-epidemiology (narrow) | 0.000 | 0.000 |
| Meta-epidemiology (broad) | 0.000 | 0.000 |
| Bibliometrics | 0.000 | 0.000 |
| Science and technology studies | 0.000 | 0.000 |
| Scholarly communication | 0.000 | 0.000 |
| Open science | 0.000 | 0.000 |
| Research integrity | 0.000 | 0.000 |
| Insufficient payload (model declined to judge) | 0.000 | 0.000 |
Machine scores (provisional)
The two teacher heads of the student model, read on this work. A score orders the frame for review; it never asserts a category, and the validation status ships verbatim with every row.
Baseline scores from an immature model (maturity gate not passed, 7 training rounds). Scores rank; they never assert a category.
score_only:v0-immature-baseline · verbatim from the scoring run: score_only means the number may rank works, and no category label ships from itClassification
machine, unvalidatedMachine predicted; a candidate call from one teacher head, not a consensus.
How this classification was reached, model by model and score by score, is at the end of the page under "How this classification was reached".