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Abanico Formation Stratigraphic range: Eocene–Miocene (typically Tinguirirican)
Type	Geological formation
Underlies	Farellones Formation
Overlies	Colimapu Formation
Thickness	ca. 3,000 m (9,800 ft)
Lithology
Primary	Volcaniclastic sediments comprising basalts, andesites & minor dacites
Other	Zeolite
Location
Coordinates	35°00′S 70°24′W / 35.0°S 70.4°W / -35.0; -70.4Coordinates: 35°00′S 70°24′W / 35.0°S 70.4°W / -35.0; -70.4
Approximate paleocoordinates	36°54′S 62°36′W / 36.9°S 62.6°W / -36.9; -62.6
Region	O'Higgins, Santiago Metropolitan & Valparaíso Regions (Chile) Mendoza Province (Argentina)
Country	Chile  Argentina
Extent	Abanico Basin
Type section
Named for	Cerro El Abanico

Abanico Formation (Spanish: Formación Abanico) is a 3 kilometres (9,800 ft) thick sedimentary formation exposed in the Andes of Central Chile.^[1] The formation has been deposited in a timespan from the Eocene to the Miocene. Abanico Formation's contact with the overlying Miocene Farellones Formation has been the subject of differing interpretations since the 1960s.^[2] A small part of the formation crops out in the Mendoza Province of western Argentina.^[3]

Description

The sediments accumulated in the Abanico Extensional Basin within a context of the Andean orogeny. The basin had a north-south elongated shape that spanned the latitudes of 29–38° S. Tectonic inversion from 21 to 16 million years ago made the basin collapse and the sediments to be incorporated to the Andean ranges.^[4] The northern part of the basin inverted before the southern part.^[2] Parts of the formation are known to have experienced Prehnite-pumpellyite facies metamorphism.^[1]

Paleontology

The Tinguiririca fauna is known from the fossils found in the Abanico Formation near the Tinguiririca River. The rich faunal assemblage of the paleontological site, located in the La Gloria Member and dated at 33 to 31 Ma, gave name to the Tinguirirican South American land mammal age (SALMA), together with the Friasian named after the Río Frías Formation of the Aysén Region, the only ages defined in Chile.^[5]

Fossil content

The following fossils have been discovered in the formation:

References

Bibliography

• 
  Charrier, Reynaldo; Luisa Pinto, and María Pía Rodríguez. 2006. 3. Tectonostratigraphic evolution of the Andean Orogen in Chile in Geology of Chile, ed. by Teresa Moreno, and Wes Gibbons, 1–326. Geological Society of London. Accessed 2018-09-08.


• 
  Godoy, Estanislao. 2012. Sobre el variable marco geotectónico de las formarciones Abanico y Farellones y sus equivalentes al ser de los 35°LS. Revista de la Asociación Geológica Argentina 69. 570–577. Accessed 2018-09-08.


• 
  Muñoz, Marcia; Luis Aguirre; Marío Vergara; Alain Demant; Francisco Fuentes, and Andrés Fock. 2010. Prehnite-pumpellyite facies metamorphism in the Cenozoic Abanico Formation, Andes of central Chile (33º50'S): chemical and scale controls on mineral assemblages, reaction progress and the equilibrium state. Andean Geology 37. 54–77. Accessed 2018-09-08.


• 
  Muñoz, Marcia; Francisco Fuentes; Mario Vergara; Luis Aguirre; Jan Olov Nyström; Gilbert Féraud, and Alain Demant. 2006. Abanico East Formation: petrology and geochemistry of volcanic rocks behind the Cenozoic arc front in the Andean Cordillera, central Chile (33°50'S). Revista Geológica de Chile 33. 109–140. Accessed 2018-09-08.

Further reading

• Charrier, R., Bustamante, M., Comte, D., Elgueta, S., Flynn, J.J., Iturra, N., Muñoz, N., Pardo, M., Thiele, R. y Wyss, A.R. 2005. The Abanico Extensional Basin: regional extension, chronology of tectonic inversion, and relation to shallow seismic activity and Andean uplift. Neues Jahrbuch für Geologie und Paläontologie Abh. 236: 43-77


• J. J. Flynn and A. R. Wyss. 2004. A polydolopine marsupial skull from the Cachapoal Valley, Andean Main Range, Chile. Bulletin of the American Museum of Natural History 285:80-92


• J. J. Flynn, A. R. Wyss, R. Charrier and C. C. Swisher. 1995. An Early Miocene anthropoid skull from the Chilean Andes. Nature 373(6515):603-607


• Fock, A., Charrier, R., Farias, M. y Muñoz, M. 2006. Fallas de vergencia oeste en la Cordillera principal de Chile: inversión de la cuenca Abanico (33°-34°S). Asociación Geológica Argentina, Serie Publicación Especial 6: 48-55


• Godoy, E., Navarro, M. y Rivera, O. 1996. Zonas triangulares en el borde occidental de la Cordillera Principal (32°30'- 34°30' l.s.), Chile: Una solución a la paradoja Abanico - Farellones 13° Congreso Geológico Argentino y 3° Congreso de Exploración de Hidrocarburos, Actas 2: 373-381, Buenos Aires


• R. B. Hitz, J. J. Flynn, and A. R. Wyss. 2006. New Basal Interatheriidae (Typotheria, Notoungulata, Mammalia) from the Paleogene of Central Chile. American Museum Novitates 3520:1-32


• M. J. Novacek, A. R. Wyss, D. Frassinetti and P. Salinas. 1989. A new ?Eocene mammal fauna from the Andean Main Range. Journal of Vertebrate Paleontology 9(3 Supp.):34A


• Vergara, M.; Morata, D.; Villarroel, R.; Nyström, J.O.; Aguirre, L. 1999. 40Ar/39Ar ages, very low grade metamorphism and geochemistry of the volcanic rocks from “Cerro El Abanico”, Santiago Andean Cordillera (33º30’S-70º25’W). In International Symposium on Andean Geodynamics, No. 4, Extended Abstracts: 785-788. Göttingen


• A. R. Wyss, J. J. Flynn, C. C. Swisher, III, R. Charrier, and M. A. Norell. 1992. Fossil mammals from the central Chilean Andes: a new interval in the South American land mammal succession, and implications for Eocene-Oligocene events and Andean tectonics. Abstracts and Program, Fifth North American Paleontological Convention 318