The Sekwi Formation in the Mackenzie Mountains, Northwest Territories, Canada is the first carbonate unit deposited during the widespread Early Cambrian transgression of the Cordilleran continental margin.  A sequence stratigraphic framework for the Sekwi Formation is established using ten detailed measured sections, each up to 1 km thick.  The Fallotaspis, Nevadella, and Bonnia-Olenellus trilobite zones provide a chronostratigraphic framework for regional and global correlations.  The lowermost sequence (S1) is an eastwardly thinning wedge, (50 to >300 m thick) composed predominantly of slope and basin deposits overlain by a thin, prograding ooid shoal complex.  The upper part of the Vampire Formation, underlying the Sekwi Formation, is included within S1.  Sequence 2 (S2; 150 to >275 m thick) includes shelf through basin deposits, whereas sequences 3 through 7 are smaller-scale sequences (40-150 m thick) with subtidal carbonate transgressive systems tracts (TSTs) and peritidal carbonate highstand systems tracts (HSTs). 

The TST of S1 consists of siliciclastic shelf deposits of the upper Vampire Formation and nodular carbonate of the lower Sekwi Formation.  The maximum flooding zone occurs within black laminated mudstone intercalated with debris flow and turbidite deposits that overly nodular carbonate.  Early HST debris flow deposits are composed predominately of slope-derived clasts with minor shelf-derived clasts.  Conversely, late HST debris flow deposits contain oolitic grainstone and subtidal shelf sandstone clasts that track progradation of an ooid shoal complex. 

The TST of S2 consists of shale and black laminated mudstone with allochthonous mud mounds.  The HST records progradation of another ooid shoal complex.