Relationship To Other Units
The Doig Formation is unconformably overlain by the Halfway Formation of the Schooler Creek Group. The contact is marked by a dolomitic bed and a chert and quartz conglomerate bed. Westwards it is overlain by newer Jurassic beds. It conformably overlays the Montney Formation, which rests under the phosphate pellet bed located in the base of the Doig.
The formation correlates with the lower Llama Member of the Sulphur Mountain Formation in the southern ranges of the Canadian Rockies, with the Whistler Member of the Whitehorse Formation in the Muskwa Ranges, and with the Toad Formation in the upper Liard River area.
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