Santa Juana Formation
Santa Juana Formation a sedimentary rock formation near Santa Juana in the lower course of Biobío River in south-central Chile. Lithologies range from conglomerate sandstone, arkosic sandstone, siltstone and mudstone.[1]
Santa Juana Formation Stratigraphic range: Carnian | |
---|---|
Type | Geological formation |
Sub-units | Talcamávida-Gomero Member Unihue Member Quilacoya Member |
Overlies | Coastal Batholith of central Chile |
Thickness | Unknown |
Lithology | |
Primary | conglomerate, sandstone, siltstone, |
Other | Arkosic sandstone, mudstone, volcanic rock, anthracite |
Location | |
Coordinates | 37.2°S 73.0°W |
Approximate paleocoordinates | 53.8°S 39.9°W |
Region | Bío Bío Region |
Country | |
Type section | |
Named for | Santa Juana |
Named by | Ferraris |
Year defined | 1981 |
Santa Juana Formation (Chile) |
Description
The sediments that consolidate into the rocks of the formation deposited in alluvial, fluvial, lacustrine and playa lake environment. Overall the formation is rich in plant fossils.[1]
The formation was deposited over the rocks of the Coastal Batholith of central Chile in a sedimentary basin that formed along the Gastre Fault. It has been posited that the basin developed as a rift during the early break-up of Gondwana in the Triassic.[1]
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See also
- Chañares Formation, fossiliferous formation of the Ischigualasto-Villa Unión Basin, Argentina
- Candelária Formation, contemporaneous fossiliferous formation of the Paraná Basin, Brazil
- Molteno Formation, contemporaneous fossiliferous formation of Lesotho and South Africa
- Pebbly Arkose Formation, contemporaneous fossiliferous formation of Botswana, Zambia and Zimbabwe
- Denmark Hill Insect Bed, contemporaneous fossiliferous unit of Queensland, Australia
- Madygen Formation, contemporaneous Lagerstätte of Kyrgyzstan
References
- Nielsen, Sven N. (2005). "The Triassic Santa Juana Formation at the lower Biobío River, south central Chile". Journal of South American Earth Sciences. 19: 547–562. doi:10.1016/j.jsames.2005.06.002.
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