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.