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- W1983931747 abstract "Bentonite chronostratigraphy indicates that deposition of the Viking Formation in central and south-central Alberta and SW Saskatchewan occurred within three chrono-intervals, informally designated Basal, Lower and Upper. Sandstone of the Basal and Lower Viking, times were deposited offshore, while most Upper Viking sands formed along the strandline. In general, these Viking sands trend NW-SE, are multiple, parallel, discrete units surrounded by swales, and are of varying thicknesses." @default.
- W1983931747 created "2016-06-24" @default.
- W1983931747 creator A5054054775 @default.
- W1983931747 date "1990-01-01" @default.
- W1983931747 modified "2023-10-02" @default.
- W1983931747 title "THE VIKING (ALBIAN) RESERVOIR SANDSTONES OF CENTRAL AND SOUTH-CENTRAL ALBERTA, CANADA Part 1. Geometry and depositional history" @default.
- W1983931747 doi "https://doi.org/10.1306/bf9ab6cd-0eb6-11d7-8643000102c1865d" @default.
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