--> Abstract: Detecting Stratigraphic Features via Cross-Plotting of Seismic Discontinuity Attributes and Their Volume Visualization, by Satinder Chopra and Kurt J. Marfurt; #90105 (2010)
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AAPG GEO 2010 Middle East
Geoscience Conference & Exhibition
Innovative Geoscience Solutions – Meeting Hydrocarbon Demand in Changing Times
March 7-10, 2010 – Manama, Bahrain

Detecting Stratigraphic Features via Cross-Plotting of Previous HitSeismicNext Hit Discontinuity Attributes and Their Volume Visualization

Satinder Chopra1; Kurt J. Marfurt2

(1) Reservoir Services, Arcis Corporation, Calgary, AB, Canada.

(2) ConocoPhillips School of Geology and Geophysics, University of Oklahoma, Norman, OK.

Fold and fault geometries, stratal architecture and large-scale depositional elements (e.g. channels, incised valley-fill and turbidite fan complexes) are often difficult to see clearly on vertical and horizontal slices through the Previous HitseismicNext Hit reflection Previous HitdataNext Hit. Consequently, visualization techniques are used for viewing the Previous HitdataNext Hit, whether it’s the input Previous HitseismicNext Hit Previous HitdataNext Hit or derived Previous HitdataNext Hit in terms of Previous HitseismicNext Hit attributes. Such visualization helps extract meaningful information, allows for greater Previous HitinterpretationNext Hit accuracy and improves efficiency. 3D volume rendering is one form of visualization that involves opacity control to view the features of interest ‘inside’ the 3D volume. A judicious choice of opacity applied to edge-sensitive attribute sub-volumes such as curvature or coherence co-rendered with the Previous HitseismicNext Hit amplitude volume can both accelerate and lend confidence to the Previous HitinterpretationNext Hit of complex structure and stratigraphy.

In addition to co-rendering, we evaluate an Previous HitinterpretationNext Hit workflow that cross-plots pairs of edge-sensitive attributes. By crossploting coherence and an appropriate curvature attribute, we can define a polygon that highlights “clusters” that exhibit low coherence (indicating a discontinuity) and high curvature (indicating folding, flexing, fault drag, or differential compaction). Modern volume Previous HitinterpretationNext Hit software allows us to link and display these interpreter-defined clusters in the Previous HitseismicNext Hit volume for further examination. Once identified interactively, such visual ‘clustering’ can be used to supervise geobody delineation using neural networks and other classification algorithms. This saves the Previous HitseismicNext Hit interpreters considerable time and effort. We illustrate this new workflow through application to several 3D Previous HitseismicNext Hit surveys recently acquired in western Canada and demonstrate that multiattribute volume co-rendering and clustering provides a powerful tool that leads to a better understanding of the spatial relationships between Previous HitseismicTop attributes and the geologic objectives being pursued.