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- W1996861232 abstract "The Flathead and Gros Ventre formations of the Teton, Gros Ventre, northwestern Wind River, and western Owl Creek Mountains gradually merge toward the east, forming the lower part of the Wyoming Deadwood; the Gallatin formation maintains its lithologic identity eastward into the Bridger Mountains, where it forms the upper part of the Wyoming Deadwood. The Gallatin contains a number of faunal zones corresponding to zones in the type St. Croixian, the lowest zone containing an early Upper Cambrian fauna. Paleontologic and stratigraphic evidence indicates that the pre-Gallatin formations are largely Middle Cambrian. The formational name, Depass, is proposed for beds lying below the Gallatin in the Wyoming Deadwood. A persistent limestone member in the lower Gros Ventre and the lower limestone member of the Gallatin are designated by the names, Death Canyon and Du Noir, respectively. The lithology, faunal content, and stratigraphic relationships of the formations are described, and an interpretation of the Cambrian history and paleogeography of Wyoming is presented." @default.
- W1996861232 created "2016-06-24" @default.
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- W1996861232 date "1936-02-01" @default.
- W1996861232 modified "2023-09-25" @default.
- W1996861232 title "Cambrian Stratigraphy of Northwestern Wyoming" @default.
- W1996861232 doi "https://doi.org/10.1086/624413" @default.
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