Quebrada del Barro Formation

The Quebrada del Barro Formation is a geological formation of the Marayes-El Carrizal Basin in San Juan Province, Argentina. This formation is the most fossiliferous portion of the Triassic Marayes Group, and is also the youngest unit of the group, overlying the El Carrizal Formation. An unconformity at the top of the Quebrada del Barro Formation separates it from the Cretaceous-age Los Riscos Formation of the El Gigante Group. Part of the formation may be made into a provincial park following the discovery of the fossils of Ingentia, a giant sauropodomorph dinosaur which helped elucidate the early evolution of sauropods.

Quebrada del Barro Formation
Stratigraphic range: Norian
TypeGeological formation
Unit ofMarayes Group
UnderliesLos Riscos Formation
OverliesCarrizal Formation
Lithology
PrimarySandstone
OtherSiltstone
Location
Coordinates31.9°S 67.2°W / -31.9; -67.2
Approximate paleocoordinates40.8°S 30.0°W / -40.8; -30.0
RegionSan Juan Province
Country Argentina
ExtentMarayes-El Carrizal Basin
Quebrada del Barro Formation (Argentina)
This article is issued from Wikipedia. The text is licensed under Creative Commons - Attribution - Sharealike. Additional terms may apply for the media files.