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- W2138101299 abstract "ABSTRACT Approximately 2700 feet of Lower and Middle Paleozoic sediments, dissected by several glacially modified canyons, crop out on the west flank of the Teton Mountains, Wyoming. Although minor amounts of shale and sandstone are present, limestone and dolomite predominate. Each of the carbonate units was thoroughly examined: samples for petrographic study were secured from those zones considered most representative of each unit. The carbonate units on the Teton's west flank are mainly fine-grained with little insoluble residue. Thin-sections show extensive dolomitization and recrystallization have destroyed much of original texture; however, enough remains to suggest that the rocks originated as calcite and/or aragonite with various allochemical associations." @default.
- W2138101299 created "2016-06-24" @default.
- W2138101299 creator A5037336475 @default.
- W2138101299 date "1965-01-01" @default.
- W2138101299 modified "2023-10-14" @default.
- W2138101299 title "Representative Carbonate Petrography Of Some Lower And Middle Paleozoic Rocks, West Flank Teton Mountains, Wyoming" @default.
- W2138101299 doi "https://doi.org/10.1306/74d7132a-2b21-11d7-8648000102c1865d" @default.
- W2138101299 hasPublicationYear "1965" @default.
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