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GCDifferential Compaction: 3-D Attributes Can Help*
Satinder Chopra1 and Kurt J. Marfurt2
Search and Discovery Article #41006 (2012)
Posted August 27, 2012
*Adapted from the Geophysical Corner column, prepared by the author, in AAPG Explorer, July, 2012. Editor of Geophysical Corner is Satinder Chopra ([email protected]). Managing Editor of AAPG Explorer is Vern Stefanic; Larry Nation is Communications Director. AAPG©2012
1 Arcis Corp., Calgary, Canada ([email protected])
2 University of Oklahoma, Norman, Oklahoma
Differential compaction has been used by seismic interpreters to map features of exploration interest such as carbonate build-ups, fans and fluvial channels. However, the 3-D mapping of compaction can take considerable time – and so many times it is not pursued.
But 3-D seismic attributes such as coherence
and curvature can be used to map compaction features. This month we illustrate the more common differential compaction expressions over paleo channels and carbonate reefs using examples from the Western Canadian Sedimentary Basin.
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Seismic attributes such as
As the name implies, "differential" compaction is a topological change due to lateral changes in the loss of rock volume as it lithifies. Channels that are filled with shale and are separated by sandier interfluves will appear as structural lows. Channels that are filled with sand cut through a shale matrix may appear as structural highs. Channels incised in older, previously compacted rock, will usually appear as lows regardless of their fill. In Figure 1 we show a chair display for a strat- In Figure 2 we show a chair display with seismic amplitude as the vertical section, and for the horizontal section we have overlaid the most-positive (red) and the most-negative curvature (blue) attributes using transparency. Notice the edges of the channel are seen in red and the axis of the channel is defined in blue. Segments of a deeper channel also are seen in the display and these have been marked with light blue arrows. In general, it is easier to reduce pore space – and therefore compact shales – than sand. If the channel is filled with sand, it will appear to have a positive relief feature seen over the length of the channel and slight negative relief feature at the edges of the channel. The Carbonates are stronger and more difficult to compact than sands and shales. While living, the carbonate mound was structurally higher than the surrounding sediments. Once it died it was covered by flat overlying, typically softer, more easily compacted sediments. Differential compaction between the reef carbonate facies and the off-reef facies results in an image whereby the overlying sediments appear to drape across the carbonate buildup. The extent of the drape would depend on the variation in the compaction of the reefal and the off-reef material as well as the thickness of the overlying sediments. In Figure 4a we show a chair display with the horizon slice from Thus, a clear understanding of the effects of differential compaction can facilitate the rapid interpretation of otherwise subtle, and perhaps otherwise overlooked geological features of interest. We thank Arcis Seismic Solutions for encouraging this work and for permission to present these results. |