Kc. Benison et Rh. Goldstein, Sedimentology of ancient saline pans: An example from the Permian Opeche Shale, Williston Basin, North Dakota, USA, J SED RES, 70(1), 2000, pp. 159-169
The mid-Permian Opeche Shale of North Dakota consists of bedded evaporites
and red-bed siliciclastics, Detailed core and petrographic study has docume
nted sedimentary and early diagenetic features in order to develop a deposi
tional model, and to refine paleoclimatic data and paleogeographic setting
for the late Paleozoic of the U.S. midcontinent.
Lithologies and sedimentary features indicate lacustrine, distal alluvial,
and minor eolian deposition, subaerial exposure, and soil formation. Bedded
halites consisting of chevron and cumulate crystals, dissolution surfaces
and pipes, and mudcracked microcrystalline salt crusts were deposited in a
saline pan dominated by flooding, evaporative concentration, and desiccatio
n, Bedded halites containing chevron and cumulate crystals but lacking any
dissolution or desiccation features formed in perennial saline lakes, Chaot
ic halite. composed of red mudstone and siltstone with displacive halite cr
ystals, represents saline mudflat deposits. Red mudstone and siltstone,vith
little or no displacive halite but with abundant cracks and root features
suggest deposition in a dry mudflat. Red-bed sandstones and conglomerates,
composed of poorly sorted, subrounded quartz grains cemented with halite in
dicate distal alluvial deposition with possible transport by ephemeral stre
ams, sheet hoods, and debris hows, Most deposition took plate in halite-dom
inated shallow perennial and ephemeral saline lakes surrounded by saline an
d dry mudflats, Evaporation, desiccation, flooding, and wind played signifi
cant roles in this environment. Therefore, the Opeche evaporites and red be
ds are representative of an ancient saline pan system.
An inland playa setting is favored as a depositional model for the Opeche S
hale. The abundance of soil features and halite dominance, as well as lack
of nearshore carbonates and lack of restricted marine fossils, suggest a cl
osed-basin nonmarine setting for the mid Permian of the U.S. midcontinent.