Botucatu Formation

Geologic formation in Brazil and Uruguay From Wikipedia, the free encyclopedia

The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment.[1] Fossil theropod tracks have been reported from the formation.[2]

Unit ofSão Bento Group
UnderliesSerra Geral Formation
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Botucatu Formation
Stratigraphic range: Aptian
TypeGeological formation
Unit ofSão Bento Group
UnderliesSerra Geral Formation
OverliesRio do Rasto Formation
Lithology
PrimarySandstone
Location
Coordinates29.7°S 52.4°W / -29.7; -52.4
Approximate paleocoordinates30.6°S 19.5°W / -30.6; -19.5
RegionRio Grande do Sul
CountryBrazil
Uruguay
ExtentParaná & Pelotas Basins
Type section
Named forBotucatu

Geologic map of the Paraná Basin with the Paleozoic and Mesozoic units in light blue
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Description

The sandstone is fine-textured and well sorted, containing no pebbles; its colour is occasionally white, yellowish, and reddish, but more commonly it is pinkish. Nearly always it is silicified and therefore compact and hard.[3] The formation was deposited in an arid desert environment, characterized by sabkhas and wadis.[4]

Fossil content

See also

References

Further reading

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