Sandstone Lithofacies Within the Icebox Fm (Ordovician), Williston
Basin, North Dakota and Montana
Aaron J. Ulishney, Department
of Geology & Geological Engineering, University of North Dakota, Grand
Forks, ND 58202, [email protected] and Richard D. LeFever,
Department of Geology & Geological Engineering, University of North Dakota,
Grand Forks, 58202.
The Icebox Fm (Ordovician) is the middle of three formations
within the Winnipeg Group. It is a regionally extensive shale, typically dark
green to black, and reaches a maximum thickness in excess of 200 ft (61 m)in
North Dakota. The Icebox contains significant organic carbon and is considered
to be an important source rock for the Lower Paleozoic in the Williston Basin.
Wireline log gamma-ray traces were digitized and
converted to a uniform scale and format. Traceable coarser facies
and discontinuities were established by correlating the digitized wireline log curves across North
Dakota and Montana.
Forty traceable sandy lithofacies were identified.
Five have regional extent, and a maximum thickness of at least 20 ft (6 m); one
is 72 ft (22 m) at its thickest. Five additional sand bodies each extend across
several tens of miles, and have maximum thicknesses ranging from 10 ft (3 m) to
23 ft (7 m).
In North Dakota,
six cores have been taken through the sandy intervals, all in the lower part of
the Icebox Fm. Based on the existing cores, it appears
that the sandy lithofacies represent intervals of bioturbated sandstone and siltstone within the shalier Icebox Fm.
The Icebox Fm in the Williston
Basin was deposited in
the epeiric sea distal to shore, but not in deep water The sandy bodies
represent environments that were somewhat shallower, perhaps even marginal
marine. Many of the less extensive bodies appear to represent deposition on top
of local topographic or structural features.