Arcadia Formation | |
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Stratigraphic range: Induan-Olenekian ~ | |
Type | Geological formation |
Unit of | Rewan Group |
Underlies | Brumby Sandstone Member |
Overlies | unconformity with Glenidal Formation conformity Sagittarius Sandstone |
Thickness | Up to 500 m (1,600 ft) |
Lithology | |
Primary | Red mudstone, siltstone, fine-grained sandstone |
Location | |
Coordinates | 24°48′S 148°00′E / 24.8°S 148.0°E |
Approximate paleocoordinates | 58°00′S 136°00′E / 58.0°S 136.0°E |
Region | Queensland |
Country | Australia |
Extent | Bowen Basin |
Type section | |
Year defined | 1988 |
The Arcadia Formation is a geological formation located within central-eastern Queensland, Australia, which has been aged between the Induan–Olenekian epoch of the Early-Triassic period. It is most well known for its abundance of Early-Triassic aged fossils, most notably its high diversity of amphibians.[1][2]