Third-order sequences

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
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During a third-order sea level change, cycle amplitude is great enough (approximately 50–150 ft) to expose the shelf. Depositional sites range from coastal plain to deep basin. The unit of strata deposited during a third-order cycle is called a depositional sequence. A depositional sequence has three subdivisions: highstand systems tract (HST), transgressive systems tract (TST), and lowstand systems tract (LST). Figure 1 shows a schematic cross section of a third-order sequence and its various systems tracts.

Third-order sequence deposition

Figure 1 . Copyright: Hyne, 1995; courtesy Tulsa Geological Society.

The schematic cross section in Figure 2 is a third-order sequence model based on observations of the Tertiary of the Gulf of Mexico passive margin basin. Although different basin types, i.e., foreland basins or active margin basins, require adjustments to the model, the Gulf of Mexico model still is useful for understanding third-order sequence deposition.

Figure 2 . Copyright: Haq, 1988; courtesy SEPM.

The order of deposition for the sequence shown in Figure 2 is as follows:

• Sequence boundary formation and lowstand systems tract; fan deposition
  • Rate of eustatic fall exceeds rate of subsidence.
  • Sea level falls to shelf break, shelf is exposed, incised; canyon cut.
  • Slope-perched deltas and submarine fans are deposited.
• Lowstand systems tract; wedge deposition
  • Rate of eustatic fall decreases, reaches a stillstand, and rises slowly.
  • Submarine fan deposition ceases.
  • Incised valleys fill with coarse-grained, low-sinuosity channel or estuarine sandstones in response to sea level rise.
  • Shale-prone wedge with thin, fine-grained turbidites forms on the slope, then downlaps the top of the submarine fan.
• Transgressive systems tract deposition
  • Rate of rise is at a maximum.
  • During brief slowdowns in the rate of rise, parasequences (fourth-order sequences) prograde; but overall they stack in a backstepping pattern.
  • Organic-rich (condensed) section moves up onto the shelf.
  • Fluvial systems typically shift from braided to meandering pattern.
• Highstand systems tract deposition
  • Rate of sea level rise is at a minimum; in the late highstand, it falls slowly.
  • Depositional rates exceed rate of sea level rise, causing parasequences to build basinward in aggradational to progradational parasequence sets.
  • Parasequences downlap onto the condensed section.

Figure 3 . Copyright: Weber et al., 1995; courtesy SEPM.

Third-order sequence example

The Desmoinian of the Paradox basin, Utah, shown in Figure 3, is an example of a third-order depositional sequence.

Figure 4 .

Carbonate platform third-order sequence

The diagrams in Figure 4 outline the deposition of a sequence associated with a carbonate plat-form during a third-order sea level cycle. Sequence deposition begins with lowstand systems tract (2 and 3) and ends with the highstand systems tract (5).

See also

• Sequence stratigraphy
• Basics of sequence stratigraphy
• Hierarchy of sequences
• Fourth- and fifth-order sequences (Parasequences)
• Traps in a framework of sequence stratigraphy

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highstand systems tract

true stratigraphic thickness, transgressive systems tract

lowstand systems tract