Lacustrian to
Fluvial Transition in the Tertiary Wasatch Formation,
Ford,
Sands of the Tertiary, Wasatch Formation
in Three Canyons of
The mouth bars are characterized by
upper-flow regime hydrodynamics with accretion towards the north-northwest,
305°. Basal bounding surfaces are inherently flat with minimal erosion; where
present, it is typically less than 0.5 meter. Horizontal planner laminations
and low-angle laminations dominate these fine grained sands. Thicknesses range
from 2 to 9 meters. Lateral to the depositional axis they grade into thin
bedded, very fine grained, ripple laminated sands and moderately bioturbated
silts and muds. These thinner beds display a downlap
geometry onto the sands of the mouth bars in the accretionary direction.
In contrast, channel forms display
multiple cut-fill cycles, typically cannibalizing their own mouth bars. They
are characterized by undulating, erosional basal surfaces with up to 5.5 meters
of scouring. They exhibit a marked grain size jump, (course-to-medium), and
clay rip-ups along their basal surfaces. Sedimentary structures include trough
cross-bedding, low-angle laminations, soft sediment deformation and ripple
laminated caps. Paleo-current indicators show an overall north-northwest, 320°,
flow. These are typically overlain by a moderately
bioturbated, silty-muds.
Characterization of this lacustrian to
fluvial transition demonstrates the complexity of what have been assumed to be
fluvial dominated sands. Understanding the variability of these systems is key to better reservoir management in analog petroleum
reservoirs.
AAPG Search and Discover Article #90063©2007 AAPG Annual Convention, Long Beach, California