Difference between revisions of "Seismic facies mapping"

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| 1 || Identify sequences that contain potential [[trap]]s, [[Seal capacity of different rock types|seal rocks]], [[Reservoir quality|reservoir rocks]], or [[source rock]]s.
| Identify sequences that contain potential [[trap]]s, [[Seal capacity of different rock types|seal rocks]], [[Reservoir quality|reservoir rocks]], or [[source rock]]s.
 
 
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| 2 || Make regional seismic reflection pattern maps and isochron maps of those sequences. If possible, make maps of [[Sea level cycle phase and systems tracts#Lowstand systems tracts|lowstand]], [[Sea level cycle phase and systems tracts#Transgressive systems tracts|transgressive]], and [[Sea level cycle phase and systems tracts#Highstand systems tracts|highstand systems tracts]].
| Make regional seismic reflection pattern maps and isochron maps of those sequences. If possible, make maps of [[Sea level cycle phase and systems tracts#Lowstand systems tracts|lowstand]], [[Sea level cycle phase and systems tracts#Transgressive systems tracts|transgressive]], and [[Sea level cycle phase and systems tracts#Highstand systems tracts|highstand systems tracts]].
 
 
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Revision as of 23:14, 19 October 2014

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Predicting the occurrence of oil and gas traps
Chapter Exploring for stratigraphic traps
Author John C. Dolson, Mike S. Bahorich, Rick C. Tobin, Edward A. Beaumont, Louis J. Terlikoski, Michael L. Hendricks
Link Web page
Store AAPG Store

Seismic facies maps show the areal distribution of seismic facies and are useful when making lithofacies interpretations. The most common and useful parameters to be mapped are seismic reflection patterns and isochrons (thickness measured in seconds of two-way time).

Procedure

The table below outlines a suggested procedure for mapping seismic facies.

Step Action
1 Identify sequences that contain potential traps, seal rocks, reservoir rocks, or source rocks.
2 Make regional seismic reflection pattern maps and isochron maps of those sequences. If possible, make maps of lowstand, transgressive, and highstand systems tracts.

Example

Figure 1 Examples of a seismic facies map, an isochron map, and seismic line A–Á (location shown on maps). Modified from Mitchum and Vail;[1] courtesy AAPG.

Figure 1 contains examples of a seismic facies map, an isochron map, and seismic line A–Á (location shown on maps).

See also

References

  1. Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, Seismic stratigraphy and global changes in sea level, part 6: Stratigraphic interpretations of seismic reflection patterns in depositional sequences, in C. E. Payton, ed., Seismic Stratigraphy and Applications to Hydrocarbon Exploration: AAPG Memoir 26, p. 117–133.

External links

find literature about
Seismic facies mapping
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