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. Dont 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