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- W2188567260 abstract "Summary Martin House and lower Arctic Red formations are sub-divided into 6 depositional sequences. Fluvial and floodplain facies of sequence 1 were deposited in a paleovalley recording a pre-existing basin geometry with drainage directed northward. Offshore marine deposits of sequence 2 were deposited in the far western part of the study area indicating that a new geometry had been established with the basin deepening westward and probably northward. From west to east sequence 3 records offshore, barrier bar, lagoon, and tidal flat deposition during relative sea level fall. The Keele Arch probably had an exposed shoreline. The base of sequence 4 is a regional ravinement surface overlain by a transgressive-regressive succession. At the base of sequence 4 the transition to offshore facies marks the base of the Arctic Red Formation in most areas. In eastern areas proximal to the Keele Arch the highstand systems tract of sequence 4 is represented by an offshore to prograding shoreface succession. Sequences 5 and 6 are generally progradational and shale westward." @default.
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- W2188567260 date "2009-01-01" @default.
- W2188567260 modified "2023-09-24" @default.
- W2188567260 title "Anatomy of a Transgressive Sandstone: Sequence Stratigraphy of the Martin House and Lower Arctic Red Formations (Albian), Peel Plateau and Plain, NWT" @default.
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