Regional cross sections of the Mannville Group in southern Alberta and Saskatchewan: Townships 1-20, Ranges 13-30W3 and Townships 1-10, Ranges 1-13W4
Authors: Vanbeselaere N A , Leckie D A , James D P , Wallace-Dudley K E 
Published: November 2010

The results of a GSC-industry, collaborative, regional mapping project of the Lower Cretaceous Mannville Group in southern Saskatchewan and Alberta (Twp. 1 - 20, Rge. 13 - 30W3 and Twp. 1 - 10, Rge. 1 - 13W4 ) are presented. The geological history is one of
multiple erosion events, creating a complexly-evolving landscape where accommodation space was generally low. We present a series of maps, cross sections and analogs to illustrate the following sequence of events.
The lowermost Cretaceous sediment (Hauterivian to Barremian) is the predominantly braided fluvial sandstones of the Sunburst/S2, deposited as a continuous, unconfined sheet directly overlying the basal Cretaceous unconformity. The top of the Sunburst/S2 is a deeply-weathered paleosol which
represents several million years of non-deposition and corresponds to a lull in tectonic activity in the Rocky Mountains.
Renewed Cordilleran tectonic activity resulted in deep incision in the eastern foreland basin, characterized by multiple episodes of incision and slow sediment supply. The result is deep incised valleys cut into pre-existing Cretaceous and older sediments. The Sunburst/S2 was preserved as erosional
remnants forming valley interfluves. The valleys are up to 75 m deep, 30 km wide and hundreds of kilometres long.
Where the incised valleys cut into Mississippian carbonates, the lowermost sediments are called the Detrital, the deposits of a landscape consisting of carbonate scarps, debris- flow deposits, talus cones, and karst features.
As relative sea level started to rise and create limited accommodation space, sediments of the Basal Quartz/McCloud were deposited on the valley floors. These quartzose reservoir sandstones were deposited as valley- confined sandy-braided rivers in Alberta, and sluggish meandering rivers in southern
Saskatchewan. Brackish to lacustrine, fine-grained sediments of the Bantry/Ostracod Member were deposited within and onlapped onto margins of the valleys. Debris flow and colluvium deposits within Bantry/Ostracod zone indicate considerable local relief, associated with nearby interfluves.
The Glauconite Member represents a complex of different facies types resulting from multiple changes in relative sea level. Shorelines and deeply incised estuarine channel deposits have been identified, opening up new exploration opportunities in Saskatchewan.
In the predominantly lithic Upper Mannville, accommodation space and sediment supply increased, changing the fluvial style to predominantly meandering with associated fine-grained floodplain deposits.
What follows are cross sections summarizing the regional geology of the Mannville Group in Twp. 1-20, Rge 13-30W3 and Twp. 1-10, Rge. 1-13W4. The cross sections were initially presented in a more generalized format to the Canadian Society of Petroleum Geologists on Tuesday, October 28, 1997, in
Calgary. This open file report is seen as supplemental data dissemination to the oral presentation.