Stratal Architecture
of the Middle Part of the Morrison Formation, Utah: Implications
for Downstream Base-Level Fluctuations
Ali-Adeeb, Riyad A.1, Timothy M. Demko1 (1) University of Minnesota Duluth, Duluth, MN
Changes in sand to mud ratios in the
fluvial deposits of the Salt Wash and Brushy Basin Members of the Upper
Jurassic Morrison Formation in south-central Utah have been attributed to
the evolution in sedimentation from a sandy, amalgamated, low-sinuosity, channel system to a muddy, non-amalgamated, moderate- to
high-sinuosity channel system. This change in depositional style is interpreted
to be a response to downstream base-level fluctuations whose origins are not
well understood. Sequence stratigraphic
interpretations are implemented to establish a high-resolution chronostratigraphic framework for the Mid-Morrison strata
in order to better correlate changes in lithology to
changing downstream base levels.
A sequence-bounding regional unconformity
separates the two members of the Morrison Formation and is characterized by overbank deposits and well-developed paleosols
that suggest extended subaerial exposure, pedogenesis, and/or possible erosion in between deposition
of the two units. Along specific localities are unique fluvial channel-fill
conglomerates that have incised into uppermost Salt Wash deposits and basal Brushy Basin deposits. These lithologically and morphologically distinct units are
characterized by a small, discontinuous and narrow lateral extent, and by red
and green chert pebble clasts.
These units are interpreted to have been deposited in small, incised paleovalleys after deposition of the lower Salt Wash Member
and prior to or concomitant with the early stages of deposition of the Brushy
Basin Member. Their unique lithology, stratigraphic position, and limited lateral continuity
suggest a previously overlooked lowstand depositional
cycle in between deposition of the Salt Wash and Brushy Basin Members.