Coimbra Group (geology)
| Coimbra Group | |
|---|---|
| Stratigraphic range: Sinemurian-Pliensbachian | |
| Type | Geological formation |
| Sub-units |
|
| Underlies |
|
| Overlies |
|
| Area | Lusitanian Basin |
| Thickness | 120-150 m |
| Lithology | |
| Primary | Limestones |
| Location | |
| Location | Coimbra Region |
| Coordinates | 39.8° N, 9.0° W |
| Region | Lusitanian Basin |
| Country | Portugal |
| Type section | |
| Named for | The Village of Coimbra |
| Named by | Dimuccio, Duarte & Cunha |
| Thickness at type section | ~120 m (390 ft) |
The Coimbra Group (Also known as Camadas de Coimbra or Calcários de S. Miguel) is a geological group of Sinemurian-Pliensbachian (Lower Jurassic) age in the Lusitanian Basin of Portugal. The unit is made of the Coimbra & the Água de Madeiros Fms, that represent a series of peritidal to intertidal facies of a Carbonate platform mostly of Obtusum-Ibex age, that gradually evolve to open marine/hemipelagic units Vale das Fontes Formation and Lemede formation. This unit is known for its fossil content, including Invertertebrate and vertebrate ichnofossils and fossils. The group wasn´t named until 2014.