Origin of the Deformed Basal Uinta Formation in Eastern Utah (Uinta Basin): Progradational Delta Clinoforms of a Lake Highstand or Ephemeral Fluvial Sheetfloods of a Lake Lowstand?
Harcourt, Nicola and David Keighley
University of New
Brunswick, Fredericton, NB
The early to middle Eocene stratigraphic succession in the Uinta
Basin can be roughly divided into a lower coarse grained unit
(Wasatch Formation), medial fine grained interval (Green River
Formation), and upper, mixed fine-coarse grained and locally
evaporitic unit (Uinta Formation). Lithofacies interpretations are of
an alluvial intermontane basin containing a major lake of fluctuating
size and depth.
The presence of saline facies in the upper part of the succession
in the west of the basin has generally lead to the conclusion that 'Lake
Uinta' gradually dried out as the basin was infilled. However, in the
east it was thought possible that there existed inclined lake-delta-front
foresets on a decameter-scale. This interpretation would indicate that
there was gradual coarse-clastic infilling of a deep lake that preceded
the onset of drier conditions.
Interpretation of basal Uinta Formation strata in the east, and the
nature of its contact with underlying shale and oil shale of the Green
River Formation, is complicated by deformation on various scales.
The localized nature of the deformations indicates their
syndepositional origin as soft-sediment deformation features. At the
meter scale, beds may be dewatered and large flame structures
punctuate the contact. At the decameter scale, domal and diapiric
mudstone structures can be viewed.
Currently, the working hypothesis is that the decameter scale
"foresets" are actually related to the large-scale domal structures, and
the beds were originally flat-lying sheetflood deposits now partly
dewatered and tilted after loading and intrusion. This suggests that the
large Uinta Lake at the time of oil shale deposition subsequently
experienced a major base-level fall before any of the observed coarser
grained units were deposited.
AAPG Search and Discovery Article #90071 © 2007 AAPG Rocky Mountain Meeting, Snowbird, Utah