Zapata Formation

Zapata Formation (Spanish: Formación Zapata) is a sedimentary formation of Lower Cretaceous age in the Magallanes or Austral Basin of Argentina and Chile. Much of the formation is folded and faulted as consequence of the Andean orogeny.[1] In outcrops of the Zapata Formation near Torres del Paine, the southernmost fossil of the ichthyosaur genus Platypterygius has been found.[2][3]

Zapata Formation
Stratigraphic range: Berriasian-Hauterivian
TypeGeological formation
UnderliesPunta Barrosa & Erezcano Formations
OverliesTobífera & Springhill Formations
Lithology
PrimaryShale
OtherTurbiditic sandstone, pyrite
Location
Coordinates51.1°S 73.3°W / -51.1; -73.3
Approximate paleocoordinates51.3°S 36.9°W / -51.3; -36.9
RegionMagallanes y la Antártica Chilena & Aysén Regions
Santa Cruz Province
Country Chile
 Argentina
ExtentMagallanes or Austral Basin
Type section
Named forCerro Zapata
Zapata Formation (Argentina)

References

  1. Fildani et al., 2008
  2. Pardo Pérez et al., 2012
  3. Páramo, 2018, p.16

Bibliography

Further reading

  • M. R. Schultz, A. Fildani, and M. Suarez. 2003. Occurrence of the southernmost South American ichthyosaur (Middle Jurassic), Parque Nacional Torres del Paine, Patagonia, southernmost Chile. Palaios 18:69-73
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