La Irene Formation

La Irene Formation
Stratigraphic range: Maastrichtian
~70–66 Ma
PreꞒ
O
S
D
C
P
T
J
K
Pg
N
TypeGeological formation
UnderliesChorrillo Formation
OverliesCerro Fortaleza Formation
Thickness230 m (750 ft)
Lithology
PrimarySandstone
OtherShale
Location
LocationPatagonia
Coordinates
La Irene Formation is located in Argentina
La Irene Formation
La Irene Formation (Argentina)

La Irene Formation is a Maastrichtian geologic formation in southern Patagonia, Argentina. The formation is 230 metres (750 ft) thick and underlies the Chorrillo Formation and rests on top of the Cerro Fortaleza Formation.[1]

Description

The formation comprises lithified, sandy sandstones and lithified, argillaceous, sandy shales deposited in a fluvial deltaic environment.

At the base of Cerro Calafate a column of about 230 metres (750 ft) in thickness was measured along the road. The 110 m below represent a succession of sandy banks clear yellowish brown color to white and dark pelitic packages fining upwards cycles are stacked to form a sequence with a clear trend growing grain and stratum. Sandy banks (coarse to fine sand) show increasing thickness from 2 m at the base to more than 9 m, whereas intercalated mudstones show an opposite trend with thickness ranging from 15 m at the base to 1 m. At the top of lower shaly packets (the thickest) are preserved carbonaceous shale intervals, thinly laminated. 120 m above correspond to a succession of amalgamated conglomeratic sandy banks where preservation is extremely rare shaly intervals.[2]

Fossil content

The formation has provided many fossil pollen of:[3]

References

  1. ^ Marenssi et al., 2003, p.406
  2. ^ La Irene Formation at Fossilworks.org
  3. ^ Povilauskas et al., 2008

Bibliography

  • Povilauskas, L.; V. Barreda, and S. Marenssi. 2008. Polen y esporas de la Formación La Irene (Maastrichtiano), sudoeste de la provincia de Santa Cruz, Argentina: primeros resultados. Geobios 41. 819-831. .
  • Marenssi, Sergio A.; Silvio Casadío, and Sergio N. Santillana. 2003. Estratigrafía y sedimentología de las unidades del Cretácico superior-Paleógeno aflorantes en la margen sureste del lago Viedma, provincia de Santa Cruz, Argentina. Revista de la Asociación Geológica Argentina 58. 403–416. Accessed 2018-08-30.