Difference between revisions of "Depositional sequence identification"

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  | part    = Critical elements of the petroleum system
 
  | part    = Critical elements of the petroleum system
 
  | chapter = Sedimentary basin analysis
 
  | chapter = Sedimentary basin analysis
  | frompg  = 4-1
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  | frompg  = 4-32
  | topg    = 4-123
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  | topg    = 4-34
 
  | author  = John M. Armentrout
 
  | author  = John M. Armentrout
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch04/ch04.htm
 
  | link    = http://archives.datapages.com/data/specpubs/beaumont/ch04/ch04.htm
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  | isbn    = 0-89181-602-X
 
  | isbn    = 0-89181-602-X
 
}}
 
}}
A [[depositional sequence]] is bounded by [[Unconformity|unconformities]] or the correlative conformity. It is subdivided by internal surfaces of [[transgression]] and [[maximum flooding]].<ref name=ch04r99>Vail, P., R., 1987, [http://archives.datapages.com/data/specpubs/oversiz2/data/a188/a188/0001/0000/0001.htm Seismic stratigraphy interpretation procedure], in Bally, A., W., ed., Atlas of Seismic Stratigraphy: [http://store.aapg.org/detail.aspx?id=478 AAPG Studies in Geology No. 1], p. 1–10.</ref><ref name=ch04r70>Mitchum, R., M., Jr., Van Wagoner, J., C., 1990, High-frequency sequences and eustatic cycles in the Gulf of Mexico basin: Proceedings, Gulf Coast Section SEPM 11th Annual Research conference, p. 257–267.</ref> Each of these surfaces is [[Chronostratigraphy|chronostratigraphically]] significant, consistently separating older strata from younger strata.
+
A depositional sequence is bounded by [[Unconformity|unconformities]] or the correlative conformity. It is subdivided by internal surfaces of [[transgression]] and [[maximum flooding]].<ref name=ch04r99>Vail, P. R., 1987, [http://archives.datapages.com/data/specpubs/oversiz2/data/a188/a188/0001/0000/0001.htm Seismic stratigraphy interpretation procedure], in A. W. Bally, ed., Atlas of Seismic Stratigraphy: [http://store.aapg.org/detail.aspx?id=478 AAPG Studies in Geology No. 1], p. 1–10.</ref><ref name=ch04r70>Mitchum, R. M., Jr., and J. C. Van Wagoner, 1990, High-frequency sequences and eustatic cycles in the Gulf of Mexico basin: Proceedings, Gulf Coast Section SEPM 11th Annual Research conference, p. 257–267.</ref> Each of these surfaces is [[Chronostratigraphy|chronostratigraphically]] significant, consistently separating older strata from younger strata.
  
 
==Identifying data==
 
==Identifying data==
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==Procedure==
 
==Procedure==
Use the table below to identify depositional sequences.
+
Use the procedure below to identify depositional sequences.
  
{| class = "wikitable"
+
# Identify depositional sequences in [[Seismic data|seismic reflection profiles]], correlating sequence boundaries throughout a data grid of seismic reflection profiles.
|-
+
# Analyze biostratigraphic data for [[Biostratigraphy in sequence stratigraphy|age-significant bioevents]] and [[Biostratigraphic correlation and age determination#Changes in abundance or composition|abundance patterns]] that may suggest depositional sequences.
! Step
+
# Analyze the depositional patterns from [[Basic open hole tools|wireline logs]], integrate the biostratigraphic data with correlated well log and [[seismic data]], and select candidate depositional sequences.
! Action
+
# Make regional stratigraphic sections by integrating seismic profile interpretations, biostratigraphic analyses, and regional well log [[cross section]]s.
|-
+
# Identify depositional sequences based on the fully integrated data set.
| 1
 
| Identify depositional sequences in [[Seismic data|seismic reflection profiles]], correlating sequence boundaries throughout a data grid of seismic reflection profiles.
 
|-
 
| 2
 
| Analyze biostratigraphic data for [[Biostratigraphy in sequence stratigraphy|age-significant bioevents]] and [[Biostratigraphic correlation and age determination#Changes in abundance or composition|abundance patterns]] that may suggest depositional sequences.
 
|-
 
| 3
 
| Analyze the depositional patterns from [[Basic open hole tools|wireline logs]], integrate the biostratigraphic data with correlated well log and [[seismic data]], and select candidate depositional sequences.
 
|-
 
| 4
 
| Make regional stratigraphic sections by integrating seismic profile interpretations, biostratigraphic analyses, and regional well log [[cross section]]s.
 
|-
 
| 5
 
| Identify depositional sequences based on the fully integrated data set.
 
|}
 
  
 
==See also==
 
==See also==
* [[Depositional sequence]]
+
 
 
* [[Definitions of depositional system elements]]
 
* [[Definitions of depositional system elements]]
 
* [[Identifying depositional sequences in seismic sections]]
 
* [[Identifying depositional sequences in seismic sections]]
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[[Category:Critical elements of the petroleum system]]  
 
[[Category:Critical elements of the petroleum system]]  
 
[[Category:Sedimentary basin analysis]]
 
[[Category:Sedimentary basin analysis]]
 +
[[Category:Treatise Handbook 3]]

Latest revision as of 21:47, 22 February 2022

Exploring for Oil and Gas Traps
Series Treatise in Petroleum Geology
Part Critical elements of the petroleum system
Chapter Sedimentary basin analysis
Author John M. Armentrout
Link Web page
Store AAPG Store

A depositional sequence is bounded by unconformities or the correlative conformity. It is subdivided by internal surfaces of transgression and maximum flooding.[1][2] Each of these surfaces is chronostratigraphically significant, consistently separating older strata from younger strata.

Identifying data

To identify depositional sequences, we use the following:

Procedure

Use the procedure below to identify depositional sequences.

  1. Identify depositional sequences in seismic reflection profiles, correlating sequence boundaries throughout a data grid of seismic reflection profiles.
  2. Analyze biostratigraphic data for age-significant bioevents and abundance patterns that may suggest depositional sequences.
  3. Analyze the depositional patterns from wireline logs, integrate the biostratigraphic data with correlated well log and seismic data, and select candidate depositional sequences.
  4. Make regional stratigraphic sections by integrating seismic profile interpretations, biostratigraphic analyses, and regional well log cross sections.
  5. Identify depositional sequences based on the fully integrated data set.

See also

References

  1. Vail, P. R., 1987, Seismic stratigraphy interpretation procedure, in A. W. Bally, ed., Atlas of Seismic Stratigraphy: AAPG Studies in Geology No. 1, p. 1–10.
  2. Mitchum, R. M., Jr., and J. C. Van Wagoner, 1990, High-frequency sequences and eustatic cycles in the Gulf of Mexico basin: Proceedings, Gulf Coast Section SEPM 11th Annual Research conference, p. 257–267.

External links

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Depositional sequence identification
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