Papo Seco Formation | |
---|---|
Stratigraphic range: Early Barremian ~ | |
Type | Geological formation |
Underlies | Assises à Orbitolines Formation |
Overlies | Porto da Calada Formation |
Lithology | |
Primary | Mudstone, siltstone |
Other | Sandstone |
Location | |
Coordinates | 38°24′N 9°12′W / 38.4°N 9.2°W |
Approximate paleocoordinates | 31°48′N 1°18′E / 31.8°N 1.3°E |
Region | Setubal |
Country | Portugal |
Extent | Lusitanian Basin |
The Papo Seco Formation is a geological formation in Portugal, whose strata date back to the Early Cretaceous.[1] Dinosaur fossils are among the fossils that have been recovered from the formation.[2][3]