Thaynes Group | |
---|---|
Stratigraphic range: Triassic | |
Type | Group |
Sub-units | Sinbad Formation, Virgin Formation, Shnabkaib Formation |
Underlies | Chinle Group |
Overlies | Kaibab Formation |
Lithology | |
Primary | Limestone |
Other | Shales, Siltstone |
Location | |
Region | Idaho, Nevada, Utah, Wyoming |
Country | United States |
Type section | |
Named by | T.H. Goodspeed |
The Thaynes Group, Thaynes Formation in older literature, is a geologic group in eastern Idaho, western Wyoming, Utah and eastern Nevada. It includes the Sinbad Formation, Virgin Formation and Shnabkaib Formation. [1] The Thaynes Group is of marine origin. Its formations are interbedded with layers of the non-marine Moenkopi Group. [1]
It preserves fossils dating back to the Early Triassic epoch (Olenekian stage). The Lower Limestone Member contains the Paris biota lagerstätte, one of the first diverse assemblages of the Mesozoic era. [2]
The Thaynes Formation is a geologic formation in Montana and Idaho, United States. It was recently elevated to group status, as the Thaynes Group.
The Alcova Limestone is a geologic formation in Wyoming. It preserves fossils dating back to the Triassic period.
The Crow Mountain Formation is a geologic formation in Wyoming. It preserves fossils dating back to the Triassic period.
The Red Peak Formation is a geologic formation in Wyoming belonging to the Chugwater Group. It preserves fossils dating back to the Triassic period.
The Gartra Formation is a geologic formation in Wyoming. It preserves fossils dating back to the Triassic period.
The Jelm Formation is a geologic formation in Wyoming. It preserves fossils dating back to the Triassic period.
The Woodside Formation is a geologic formation in Wyoming. It preserves fossils dating back to the Triassic period.
The Martin Bridge Formation is a geologic formation in Idaho. It preserves fossils dating back to the Triassic period.
The Salt Lake Formation is a geologic formation exposed principally in Northern Utah and Southeast Idaho, with other small exposures in Southwest Wyoming and Northeast Nevada. Dates generally range from mid-Miocene to early Pliocene, with most dates falling between 10 Ma to 4 Ma, but perhaps starting as early as 15 Ma and extending to as late as 2 Ma in places. The primarily sedimentary record preserves lacustrine and alluvial fan environments, as well as a few tuffaceous expressions. Preserved fossils include Blancan fauna.
The Curtis Formation is a geologic formation in Utah. It preserves fossils dating back to the Callovian age of the Jurassic period.
The Virgin Formation is a geologic formation in Utah. It preserves fossils dating back to the Triassic period.
The Osobb Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Prida Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Priada Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Augusta Mountain Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Dun Glen Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Excelsior Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Grantsville Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Hoyt Canyon Formation is a geologic formation in Nevada. It preserves fossils dating back to the Triassic period.
The Spray River Group is a stratigraphic unit of Triassic age. It is present on the western edge of the Western Canada Sedimentary Basin in the foothills and Rocky Mountains of western Alberta. It was originally described as the Spray River Formation by E.M. Kindle in 1924 and was later raised to group status. Its type section is located in the Spray River gorge at the southern end of Sulphur Mountain.