Griman Creek Formation
The Griman Creek Formation is a geological formation in northern New South Wales and southern Queensland, Australia whose strata date back to the Albian-Cenomanian stages of the mid-Cretaceous. It is most notable being a major source of opal, found near the town of Lightning Ridge, New South Wales. Alongside the opal opalised fossils are also found, including those of dinosaurs and primitive monotremes.
Griman Creek Formation | |
---|---|
Stratigraphic range: late Albian-early-mid Cenomanian ~ | |
Type | Geological formation |
Unit of | Rolling Downs Group |
Sub-units | Coocoran Claystone & Wallangulla Sandstone Members |
Underlies | Unconformity with Oligo-Miocene Cumborah Gravel |
Overlies | Surat Siltstone, Wallumbilla Formation |
Thickness | Up to 345 m (1,132 ft) |
Lithology | |
Primary | Sandstone, siltstone, mudstone |
Other | Conglomerate, coal |
Location | |
Coordinates | 29.4°S 147.7°E |
Approximate paleocoordinates | 64.4°S 134.9°E |
Region | Queensland New South Wales |
Country | Australia |
Extent | Surat Basin |
Type section | |
Named for | Griman Creek |
Named by | Reiser |
Year defined | 1970 |
Griman Creek Formation (Australia) |
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.