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Chilenia

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Ancient microcontinent, containing central Chile and western Argentina
Geology of the Andes
Orogenies
Fold-thrust belts
Batholiths
Subducted structures
Faults
Andean Volcanic Belt
Pampean flat-slab
Terranes

Chilenia was an ancient microcontinent or terrane whose history affected many of the older rocks of central Chile and western Argentina. It was once separated by oceanic crust from the Cuyania terrane to which it accreted at ~420-390 Ma when Cuyania was already amalgamated with Gondwana.

See also

  • Andes – Mountain range in South America

References

  1. Rapalini, A.E. 2005. The accretionary history of southern South America from the latest Proterozoic to the Late Palaeozoic: some palaeomagnetic constraints. From: Vaughan, A. R M., Leat, P. T. & Pankhurst, R. J, (eds). Terrane Processes at the Margins of Gondwana. Geological Society, London, Special Publications, 246, 305-328.

Sources

Geology of Chile
Terranes
Sedimentary
formations
and groups
Cenozoic
Neogene
Paleogene
Mesozoic
Cretaceous
Jurassic
Triassic
Paleozoic
Batholiths
Metamorphic
complexes
Faults
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