Difference between revisions of "Seismic facies mapping"

From AAPG Wiki
Jump to navigation Jump to search
(Initial import)
 
 
(14 intermediate revisions by 2 users not shown)
Line 6: Line 6:
 
  | part    = Predicting the occurrence of oil and gas traps
 
  | part    = Predicting the occurrence of oil and gas traps
 
  | chapter = Exploring for stratigraphic traps
 
  | chapter = Exploring for stratigraphic traps
  | frompg  = 21-1
+
  | frompg  = 21-40
  | topg    = 21-68
+
  | topg    = 21-40
 
  | author  = John C. Dolson, Mike S. Bahorich, Rick C. Tobin, Edward A. Beaumont, Louis J. Terlikoski, Michael L. Hendricks
 
  | author  = John C. Dolson, Mike S. Bahorich, Rick C. Tobin, Edward A. Beaumont, Louis J. Terlikoski, Michael L. Hendricks
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch21/ch21.htm
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch21/ch21.htm
Line 14: Line 14:
 
  | isbn    = 0-89181-602-X
 
  | isbn    = 0-89181-602-X
 
}}
 
}}
Seismic fades maps show the areal distribution of seismic fades 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).
+
[[Basics of seismic facies analysis|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 sequence analysis|seismic reflection patterns]] and [[isochron]]s (thickness measured in seconds of two-way time).
  
 
==Procedure==
 
==Procedure==
The table below outlines a suggested procedure for mapping seismic fades.
+
The steps below outlines a suggested procedure for mapping seismic facies.
  
{| class = "wikitable"
+
# Identify sequences that contain potential [[trap]]s, [[Seal capacity of different rock types|seal rocks]], [[Reservoir quality|reservoir rocks]], or [[source rock]]s.
|-
+
# 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]].
! 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==
 
==Example==
The figure below contains examples of a seismic fades map, an isochron map, and seismic line A–Á (location shown on maps).
 
  
[[file:exploring-for-stratigraphic-traps_fig21-28.png|thumb|{{figure number|21-28}}Modified.]]
+
[[file:exploring-for-stratigraphic-traps_fig21-28.png|300px|thumb|{{figure number|1}}Examples of a seismic facies map, an isochron map, and seismic line A–Á (location shown on maps). Modified from Mitchum and Vail;<ref>
 +
Mitchum, R. M., P. R. Vail, and J. B. Sangree, 1977, [http://archives.datapages.com/data/specpubs/seismic1/data/a165/a165/0001/0100/0117.htm 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: [http://store.aapg.org/detail.aspx?id=1157 AAPG Memoir 26], p. 117–133.</ref> courtesy AAPG.]]
 +
 
 +
[[:file:exploring-for-stratigraphic-traps_fig21-28.png|Figure 1]] contains examples of a seismic facies map, an [[isochron]] map, and seismic line A–Á (location shown on maps).
  
 
==See also==
 
==See also==
* [[Facies analysis]]
+
* [[Seismic facies analysis]]
 
* [[Basics of seismic facies analysis]]
 
* [[Basics of seismic facies analysis]]
 
* [[Reflection configuration patterns]]
 
* [[Reflection configuration patterns]]
Line 44: Line 37:
 
* [[Analyzing lithofacies]]
 
* [[Analyzing lithofacies]]
 
* [[Petrophysical analysis of lithofacies]]
 
* [[Petrophysical analysis of lithofacies]]
 +
 +
==References==
 +
{{reflist}}
  
 
==External links==
 
==External links==
Line 52: Line 48:
 
[[Category:Predicting the occurrence of oil and gas traps]]  
 
[[Category:Predicting the occurrence of oil and gas traps]]  
 
[[Category:Exploring for stratigraphic traps]]
 
[[Category:Exploring for stratigraphic traps]]
 +
[[Category:Treatise Handbook 3]]

Latest revision as of 17:47, 4 February 2022

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 steps below outlines a suggested procedure for mapping seismic facies.

  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