J. Melvin, EVOLVING FLUVIAL STYLE IN THE KEKIKTUK FORMATION (MISSISSIPPIAN), ENDICOTT FIELD AREA, ALASKA - BASE-LEVEL RESPONSE TO CONTEMPORANEOUS TECTONISM, AAPG bulletin, 77(10), 1993, pp. 1723-1744
Citations number
43
Categorie Soggetti
Energy & Fuels",Geology,"Geosciences, Interdisciplinary
The hydrocarbon reservoir at Endicott field, offshore from the Sagavan
irktok delta in northeastern Alaska, is found in the Upper Mississippi
an (Visean) Kekiktuk Formation. The trap is bounded by the northwest-s
outheast-trending Tigvariak and Mikkelson Bay faults, and the younger
east-west-trending Niakuk fault. The Kekiktuk comprises sandstones, si
ltstones, and mudstones with locally significant coals and conglomerat
es, and is subdivided into three major reservoir zones based on the re
lative dominance of these lithologies. Zone 1 (the lowest) comprises m
udstones, siltstones, and coals with subordinate isolated sandstones,
and represents deposition within a low-lying swamp plain. With very lo
w net-to-gross ratio, this zone is considered to be effectively nonres
ervoir. Major movement on the Mikkelson Bay and Tigvariak faults creat
ed a half-graben with uplift to the north and east and a very signific
ant drop in base level. This change resulted in fairly widespread depo
sition of zone 2, medium- to coarse-grained sandstones from sandy bed-
load braided streams. However, those sandstones thin significantly to
the west, away from the faults. Continuing tectonism at this time crea
ted local shifts in base level, manifest as diversion of streams wides
pread abandonment, and subsidence leading to the creation of a large l
ake. The lacustrine deposits are widespread, and effectively divide zo
ne 2 into two subzones. Those subzones are mappable sheet sandstones,
and constitute the best reservoir at Endicott field in terms of net-to
-gross ratio, porosity/permeability, and sandstone connectivity. Base
level shows evidence of rising dramatically at the end of zone 2. This
rise is attributed to continuing tectonism within the basin, and is p
articularly associated with the east-west-trending mid-field fault sys
tem at Endicott field, as well as ongoing activity on the Tigvariak/Mi
kkelson Bay fault system. Thus, at the base of zone 3 (subzone 3A), in
the southern and eastern parts of the field, the rocks are mudstones
and widespread coals, and contain at least one unequivocally marine mu
dstone. These rocks are lower delta-plain interdistributary bay-fill d
eposits, with rare distributary channel sandstones. North and west of
the mid-field fault system, the marine mudstone is absent and the faci
es changes significantly with the loss of dominant coal and a concomit
ant increase of distributary channel sandstones. Reservoir properties
of subzone 3A, including connectivity, are significantly different in
this area. Subzone 3B is a thick accumulation of fine-grained alluvial
overbank deposits within which occur rare, isolated anastomosed chann
el sandstones of limited connectivity. This subzone makes minimal cont
ribution to Endicott field reserves. Subzone 3C is characterized (part
icularly in its upper part) by well-developed fining-upward cycles ind
icating mature meandering streams. The relationships between these two
highest subzones of the Kekiktuk at Endicott field indicate they repr
esent an aggradational episode initiated by tectonically induced avuls
ion and set against a background of rising base level. To the west, at
some distance from the Tigvariak/Mikkelson Bay fault system, zone 3 i
s much thinner than at Endicott field, and is dominated by mudstones a
nd coals. This evidence emphasizes the control that contemporaneous te
ctonism related to those faults had on sediment (especially sandstone)
distribution within the Kekiktuk Formation. Base level changes can be
identified within the Kekiktuk Formation in the North Slope subsurfac
e by careful lithofacies analysis and an awareness of key constraining
indicators, such as are revealed by palynology, paleontology, and str
uctural geology. By analogy with shallow-marine rocks, sequence strati
graphic concepts may be extended to continental successions. However,
one must approach such problems with a full awareness of the impact of
tectonism on base level and basin development.