Madre de Dios Terrane
Madre de Dios Terrane is a distinct
- Denaro Complex
- Torlton Limestone
- Duque de York Complex is made up of pelites, greywackes and conglomerates. All these sediments are thought to be derived from a continent or microcontinent. Duque de York Complex was metamorphosed before the Cretaceous intrusions of the South Patagonian Batholith, as is also likely the case of the two other units.
References
- ^ a b Sepúlveda, S.A.; Hervé, F.; Calderón, M.; Lacassie, J.P. (2008). "Petrological and geochemical characteristics of metamorphic and igneous units from the allochthonous Madre de Dios Terrane, Southern Chile". Gondwana Research. 13 (2): 238–249.
