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Pardonet Formation : ウィキペディア英語版 | Schooler Creek Group
The Schooler Creek Group is a stratigraphical unit of Ladinian to Norian age in the Western Canadian Sedimentary Basin. It was named for ''Schooler Creek'', a left tributary of the Williston Lake, and was first described north-west of Fort St. John in the ''Pacific Fort St. John No. 16'' and ''Southern Production No. B-14-1'' wells by F.H. McLearn in 1921.〔McLearn, F.H., 1921. Mesozoic of upper Peace River, British Columbia Geological Survey of Canada, Summary Report 1920, Part B, p. 1-6.〕 ==Lithology== The Schooler Creek Group is composed of limestone and dolostone, with subordinate siltstone, shale, sandstone and evaporite.
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