Carbonate Sequence Stratigraphy and Field Examples:
Fundamentals of Carbonate Sequence Stratigraphy

Charles Kerans
Scott W. Tinker

Bureau of Economic Geology

 
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The components of sequence stratigraphy
Cycles
Cycle Sets
Systems Tracts
High Frequency Sequences
Composite Sequences
Defining a hierarchy of cyclicity is a fundamental but often poorly conducted step in constructing a stratigraphic framework. The construction of this hierarchy must be done as a conscious effort and must include data that many times is considered non-standard for reservoir characterization. For example, many carbonate core descriptions recognize cycle tops only where tidal-flat lithofacies are present, leaving all subtidal cycles uninterpreted. This can create an inconsistent view of the cycle hierarchy, with a few very thick cycles and a few very thin cycles and no transitional cycles. Establishing a stratigraphic hierarchy must entail looking at both big picture and detailed data Building a robust sequence framework does not necessarily save time up front, but instead gives a more predictive and useful end result, and perhaps saves time and money in the long run.

The terminology advocated for cyclostratigraphy is a relative one. In two-dimensional sequence parlance, the terms applied here are composite sequence, high-frequency sequence, and cycles. In the one-dimensional world of cyclostratigraphy this hierarchy tends to be a numbered order system (1st = longest term, 5th = shortest term) (Fig. I). In most Precambrian through early Cenozoic data sets it is not possible to constrain the time element sufficiently to determine the average cycle duration. Still, most workers find that a first-pass evaluation of their cycle hierarchy in terms of this stratigraphic ordering is a useful exercise. As better resolution techniques for absolute dating of stratigraphic successions become available, it will be possible to improve the current technique of finding upper and lower bounding surfaces that are loosely constrained radiometrically and dividing the elapsed time implied by the number of cycles in the interval to arrive at a average cycle duration.
Definition
Cycle:
(5th order) The fundamental building block of carbonate stratigraphic analysis. Refers to the smallest set of genetically related facies deposited during a single base level rise/fall event. Comparable to parasequence. Can be mapped across multiple facies tracts, as distinguished from autocycles.
Tinker, JSR (1997)
Above: the hierarchy of cyclicity as preserved in carbonate settings, beginning with the cycle, the fundamental building block of carbonate stratigraphy. Cycles are usually on the order of 1-5 meters thick and are indicativeof predictable changes in water depth and water energies. Cycles bundled together - usually in groups of 2 to 5 - form cycle sets which can be interpreted across multiple facies tracts, shown here from shelf crest into a basin. Cycles sets (shown in yellow) are components of high frequency sequences (shown in blue) which may be made up of 3 to 7 cycle sets. High frequency sequences are components of composite sequences.
 
Transposed onto a analog outcrop (below), the same cycle history can be clearly identified. Beginning with a basal mudstone up through burrowed peloid packstone indicating a dominantly below-fair-weather wave base environment, to bedded peloid grainstones and grain-dominated packstones into ooid stratified grainstones above-fair-weather wave base, and finally, a fenestral algal laminated cycle cap. This rock record, approximately 15 feet thick, represents a single cycle. Geologically, there is great variability in permeability in these cycles: mudstones tend to be very tight, low permeability rocks while the higher-energy facies can have permeability variation that is quite significant. Understanding reservoir performance is possible by working out the architecture of the cyclicity and mapping out relative geometries of mudstones versus other carbonate rocks in a larger area.
Although perm varies greatly in carbonate rocks, cycle bases are commonly mud or clay rich, and very tight (low perm). Interpreting the correct cycle hierarchy becomes critical for understanding reservoir-scale heterogeneity.

Process of Facies Description in Outcrop and Core

Facies (4-10 facies for log and seismic ties)
• Lithology
• Texture
• Grains
• Pore Types
Depositional Environment/Water Depth
Cyclicity/Stratigraphy
Sequences and flooding surfaces identified


It all starts with the rocks:
facies description is critical to the interpretive process. This requires using core sample or outcrop data to identify several key indicator facies - 4 or 5 may be sufficient - to map component architecture. Three critical environments to identify by key lithofacies include: sea-level interface, above fair-weather wave base, and below fair-weather wave base. Some combination of lithology, texture, grain type, or pore type will help to determine the depositional environment or water depth. The vertical organization of those rocks, depositional environments, or accommodation cycles, through time allows us to interpret cyclicity and stratigraphy, and makes possible the interpretation of longer term High Frequency Sequences and composite sequence.

Definition

Cycle Set: Bundles of cycles that show a consistent stratigraphic trend, either progradational, aggradational, or retrogradational (transgressive). Comparable to parasequence set.

 
CYCLE SETS

Cycle sets are bundles of cycles that show a consistent trend, either progradational, aggradational, or retrogradational transgressive (above). Cycle set is analogous to Van Wagoner et als. (1990) parasequence set. In many reservoirs such as the Leonardian Clear Fork of the Permian Basin, this cycle set level is critical for reservoir framework construction as the individual cycles are of insufficient thickness/log response to be mapped (Holtz et al. 1992), and may not have impact on reservoir production.

 

Above: An outcrop photograph revealing four cycles. Mudstones at the base of each cycle are clearly visible in gray, with increasing grain composition (decreasing mud) upward to higher energy environments at the top, then repeating. This stack is a thinning upward succession of cycles that are part of a larger cycle set. Again, mudstones tend to interrupt vertical fluid flow in the subsurface as demonstrated in an illustration of flow simulation of an outcrop section. The water injector on the left (shown in blue) and the producing well on the right (fluids shown in red) illuminate key differences in architecture, with base cycles being very tight and higher energy grainstones being swept more efficiently. Architecture of the reservoir is controlled primarily by mudstones and grainstones which determine reservoir compartmentalization as well as the heterogeneity of the reservoir system. Though this example is relatively flat, in regions of greater accommodation such systems tend to prograde or backstep and reveal more complex stratal geometry. For this reason it is very important to work out the stratal geometry and reservoir archictecture to achieve an accurate 3-D reservoir model.

Definition

High-Frequency Sequence: A (4th order) High-Frequency Sequence (HFS) is bound at its top and base by unconformities or their correlative conformities, and composed of systems tracts defined by base-level fall (LST), base-level rise (TST), and base level fall (HST) successions.

 

HIGH FREQUENCY SEQUENCES

By definition a depositional or composite sequence consists of "a relatively conformable succession of genetically related strata bounded at its top and base by unconformities or their correlative conformities" (Mitchum et al.1977). Mitchum and Van Wagoner (1991) recognized, through detailed stratigraphic analysis of core and well log data, that classic Vail-type depositional sequences originally delineated predominantly from seismic data are made up of multiple unconformity-bounded sequences. Mitchum and Van Wagoner (1991) proposed the term composite sequence for those depositional sequences that are comprised of multiple unconformity-bound sequences. The term high-frequency sequence was designated for these higher-frequency unconformity-bound sequences within the larger composite sequence. High-frequency sequences may have all of the attributes of composite sequences, including lowstand, transgressive, and highstand systems tracts and their component cycles and cycle sets.

Definition

Composite Sequence: (Depositional Sequence, 3rd order) is a relatively conformable succession of genetically related strata, bound at its top and base by unconformities or their correlative conformities, and often composed of multiple unconformity-bound High-Frequency Sequences (HFS).

COMPOSITE SEQUENCES

Whereas high-frequency sequences can be divided into systems tracts composed of retrogradational and progradational cycle sets, systems tract delineation in composite sequences uses comparable sets of high-frequency sequences, or sequence sets (lowstand, transgressive, and highstand). Both high-frequency and composite sequences are bounded by base-level-fall to base-level-rise turn-arounds, which can be manifested in several ways. Bounding surfaces of high-frequency sequences are identified on the basis of 1) subaerial unconformities and karstification, 2) a turn-around from progradational to retrogradational cycles (i.e., two-dimensional cycle stacking patterns), 3) major basinward shifts or offsets in the location of lithofacies tracts across a single surface, an extreme example of which would be a downward shift of coastal onlap onto the slope, and 4) analysis of systematic trends in the thickness and lithofacies proportion of cycles, commonly referred to as stacking pattern analysis (upward thickening and upward deepening cycles during base-level rise followed by upward thinning and upward shallowing to a sequence boundary during base-level fall).

High-frequency sequences can be divided into systems tracts in a manner identical to that outlined originally for depositional sequences (Vail, 1987). Transgressive and highstand systems tracts can be recognized for all high frequency sequences through delineation of retrogradational, aggradational, and progradational cycle sets (cf. parasequence sets of Van Wagoner et al.1988,1990).

Key Elements of System Tracts

Systems Tracts: Lowstand, Transgressive, and Highstand Systems Tracts are recognized by delineation of retrogradational, aggradational, and progradational cycle sets and component facies.

Transgressive Systems Tracts:
•Bounded below by underlying sequence boundary and above by maximum flooding surface
•Generally more mounded in geometry
•Sets of high-frequency cycles show upward thickening and upward deepening trends
•Typically less grainstone prone, more diverse skeletal assemblages
Highstand Systems Tracts:
• Bounded below by maximum flooding surface and above by overlying sequence boundary
• Generally shingled or offlapping (clinoformal) stratal geometry
• Sets of high-frequency cycles show upward thinning and upward shallowing trends
• Typically grainstone prone, less diverse skeletal assemblages
Lowstand Systems Tracts:
• under-studied in carbonate systems

Definitions

Maximum Flooding Surface:
• Surface that marks the turn-around from landward-stepping to seaward stepping strata
• Farther out on platform coincides with the downlap surface (depending on the degree of condensation of clinoform toes)
• Recognition of the MFS is important for separating TST and HST, which in turn is important for other stratigraphic analysis, but on the platform top (where a very large percentage of carbonate reservoirs occur) this can be difficult to pin down precisely. Don’t get hung up on this. Try to pick it as closely as possible, knowing that your colleague will disagree in order to appear enlightened.

Sequence Boundary:
• The unconformity or correlative conformity that bounds a sequence
• Not always a major physical feature
• Not every exposure surface is a sequence boundary!
• Commonly (but not always) represents a significant change in stratal arrangements and therefore reservoir properties

 

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