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Abanico Formation
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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]

Key Information

Description

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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]

Paleontological significance

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References

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Further reading

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