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• W2000306403 abstract "Research Article| June 01, 2008 Stratigraphy and facies of Cambrian to Lower Ordovician strata in Saskatchewan James Dixon James Dixon Geological Survey of Canada 3303 – 33 Street NW Calgary, AB T2L 2A7 Search for other works by this author on: GSW Google Scholar Bulletin of Canadian Petroleum Geology (2008) 56 (2): 93–117. https://doi.org/10.2113/gscpgbull.56.2.93 Article history received: 17 Dec 2007 accepted: 06 May 2008 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation James Dixon; Stratigraphy and facies of Cambrian to Lower Ordovician strata in Saskatchewan. Bulletin of Canadian Petroleum Geology 2008;; 56 (2): 93–117. doi: https://doi.org/10.2113/gscpgbull.56.2.93 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyBulletin of Canadian Petroleum Geology Search Advanced Search Abstract Cambrian to Lower Ordovician strata in Saskatchewan are present only in the subsurface and are mostly siliciclastic. They are divided into three units which, in ascending order, are the informally named Basal Sandstone Unit overlain by the Earlie Formation and Deadwood Formation. Strata of the Basal Sandstone Unit and Earlie Formation are Middle Cambrian and those of the Deadwood Formation range from the Upper Cambrian to Lower Ordovician. Sedimentary facies indicate that all units were deposited in environments ranging from shoreface to shallow-water shelf.Two major transgressive-regressive sequences are identified in these strata; the older is comprised of the Basal Sandstone Unit and most of the Earlie Formation, and the younger one is mostly the Deadwood Formation. The boundary between the two sequences shows very little evidence of erosion but the younger sequence overlaps the older sequence in an easterly direction. The upper boundary of the younger sequence is a major erosional surface. Facies trends in the sequences indicate an eastern to northeastern source of the siliciclastic sediment. The Saskatchewan succession is comparable to similar age strata in north-central and western USA, and the Interior Plains of Western Canada and the Northwest Territories.Many sandstone beds in the succession are porous and would be suitable petroleum reservoirs but the source rock potential of the associated shale appears poor. However, the reported presence of Gloeocapsomorpha sp., a fossil with known hydrocarbon-producing potential, could be a positive indicator if it can be found concentrated in organic-rich laminae or thin beds. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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• W2000306403 date "2007-06-01" @default.
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• W2000306403 title "Stratigraphy and facies of Cambrian to Lower Ordovician strata in Saskatchewan" @default.
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