Sequences, Systems Tracts, and Eustatic Cycles
Henry W. Posamentier and Peter R. Vail
Depositional sequences are composed of genetically related sediments bounded
by unconformities
or their correlative conformities and are related to cycles of
eustatic change. The bounding
unconformities
are inferred to be related to
eustatic fall inflection points. They will be either Type 1 or Type 2
unconformities
depending on whether sea level fall was rapid (i.e., rate of
eustatic fall exceeded subsidence rate at the depositional shoreline break) or
slow (i.e., rate of eustatic fall was less than subsidence rate at the
depositional shoreline break). Each sequence is comprised of a succession of
systems tracts. Four systems tracts are recognized: lowstand, transgressive,
highstand, and shelf margin systems tracts. The lowstand systems tract is
subdivided into two parts lowstand fan and lowstand wedge where the basin margin
is characterized by a discrete physiographic shelf edge, or lower and upper
wedge where the basin margin is characterized by a ramp physiography. Each
systems tract is comprised of a linkage of contemporaneous depositional systems.
Type 1 and Type 2 unconformities
are each characterized by a basin-ward shift
of coastal onlap concomitant with a cessation of fluvial deposition. The style
of subaerial erosion characterizing each unconformity is different. Type 1
unconformities
are characterized by stream rejuvenation and incision, whereas
Type 2
unconformities
typically are characterized by widespread erosion
accompanying gradual denudation or degradation of the landscape. Stream
rejuvenation and incision are not associated with this type of unconformity.
On the slope and in the basin, Type 1 unconformities
typically are overlain
by lowstand fan or lowstand wedge deposits, whereas Type 2
unconformities
are
overlain by shelf-margin systems tract deposits. Within incised valleys on the
shelf, Type 1
unconformities
are overlain by either fluvial (lowstand wedge) or
estuarine (transgressive) deposits. Type 2
unconformities
typically are
characterized by a change in parasequence stacking pattern from progradational
to aggradational.
AAPG Search and Discovery Article #91030©1988 AAPG Annual Convention, Houston, Texas, 20-23 March 1988.