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Autor:
Gonzalo Blanco, Paulina Abre, Mabel Lanfranchini, Carlos A. Cingolani, Hector Ferrizo, Daniel Piñeyro, Norberto J. Uriz, Manuela E. Benítez
Publikováno v:
Agrociencia Uruguay, Vol 26, Iss NE1, p e525 (2022)
The geochemistry of two metavolcano-sedimentary sequences deposited in the Piedra Alta Terrane is compared, and their geotectonic evolution is discussed. The Ojosmín Unit (OU) comprises MORB-like basic rocks at the base and a fine-grained siliciclas
Externí odkaz:
https://doaj.org/article/9001c271085e4b3eb1ac204e685c9962