Difference between revisions of "Traps in a framework of sequence stratigraphy"
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==Shelf-edge and ramp-type margin traps== | ==Shelf-edge and ramp-type margin traps== | ||
| − | [[:file:exploring-for-stratigraphic-traps_fig21-15.png|Figure 2]] shows two schematic [[cross section]]s showing potential [[Stratigraphic trap|stratigraphic]] and [[Combination trap|combination stratigraphic-structural plays]] associated with [[Basics of sequence stratigraphy|sequences]] and [[Parasequences (fourth- and fifth-order sequences)|parasequences]] on [[Lithofacies_and_environmental_analysis_of_clastic_depositional_systems#Clastic_depositional_lithofacies_and_environments|shelf-edge and ramp margins]]. Shelf-edge margins are found in continental margin basins. Ramp margins are found in cratonic, continental margin, or [[Lithofacies_and_environmental_analysis_of_clastic_depositional_systems#Lacustrine_deposits|lacustrine basins]]. The numbers in the cross sections correspond to the numbers in the table. | + | [[:file:exploring-for-stratigraphic-traps_fig21-15.png|Figure 2]] shows two schematic [[cross section]]s showing potential [[Stratigraphic trap|stratigraphic]] and [[Combination trap|combination stratigraphic-structural plays]] associated with [[Basics of sequence stratigraphy|sequences]] and [[Parasequences (fourth- and fifth-order sequences)|parasequences]] on [[Lithofacies_and_environmental_analysis_of_clastic_depositional_systems#Clastic_depositional_lithofacies_and_environments|shelf-edge and ramp margins]]. Shelf-edge margins are found in [[continental margin]] basins. Ramp margins are found in cratonic, continental margin, or [[Lithofacies_and_environmental_analysis_of_clastic_depositional_systems#Lacustrine_deposits|lacustrine basins]]. The numbers in the cross sections correspond to the numbers in the table. |
==See also== | ==See also== | ||
Revision as of 20:55, 20 November 2015
| 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 |
Play types
Figure 2 Two schematic cross sections showing potential stratigraphic]] and [combination stratigraphic-structural plays associated with sequences and parasequences on shelf-edge and ramp margins. After Van Wagoner et al.[3]
The schematic cross section (Figure 1) illustrates different stratigraphic play types in the context of sequence stratigraphy.
Shelf-edge and ramp-type margin traps
Figure 2 shows two schematic cross sections showing potential stratigraphic and combination stratigraphic-structural plays associated with sequences and parasequences on shelf-edge and ramp margins. Shelf-edge margins are found in continental margin basins. Ramp margins are found in cratonic, continental margin, or lacustrine basins. The numbers in the cross sections correspond to the numbers in the table.
See also
- Sequence stratigraphy
- Hierarchy of sequences
- Third-order sequences
- Fourth- and fifth-order sequences (Parasequences)
References
- ↑ Baum, G. R., Vail, P. R., 1988, Sequence stratigraphic concepts applied to Paleogene outcrops, Gulf and Atlantic basins, in Wilgus, C. K., Hastings, B. S., Posamentier, H. M., Van Wagoner, J., Ross, C. A., Kendall, G. C. St. C., eds., Sea-Level Changes—An Integrated Approach: SEPM Special Publication 42, 407 p.
- ↑ Sarg, J. F., 1988, Carbonate sequence stratigraphy, in Wilgus, C. K., Hastings, B. S., Posamentier, H. M., Van Wagoner, J., Ross, C. A., Kendall, G. C. St. C., eds., Sea-Level Changes—An Integrated Approach: SEPM Special Publication 42, p. 155–181.
- ↑ Van Wagoner, J. C., Mitchum, R. M., Campion, K. M., Rahmanian, V. D., 1990, Siliciclastic Sequence stratigraphy in Well Logs, Cores and Outcrops: Concepts for High-Resolution Correlation of Time and Facies: AAPG Methods in Exploration Series No. 7, 55 p.
External links
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