Abstract
Quealy Dome, Albany County, Wyoming, is an asymmetric Rocky Mountain foreland fold on the west flank of the Laramie basin. Production is from the Lower Cretaceous Muddy Sandstone and Dakota Sandstone and from the Jurassic Sundance Formation and Permian-Pennsylvanian Casper Formation. Accumulation is structurally controlled. Internal structure of the fold involves "out-of-the-syncline" thrusting and post-folding normal faulting.
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