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- W129336873 abstract "Southern Andes: accretionary history of the basement blocks The composition and distribution of Andean magmas are strongly influenced by the age and extent of the different basement blocks beneath the modern Andes. In particular, radical revision of southwestern Gonwana assembly models depicted in recent studies has to be taken into account when considering the variation with time of the early pre-Andean and Andean subduction-related granitic magmas (Fig. 1): (i) Palaeomagnetic studies indicate that one of the most important assembly episodes occurred during the Pampean-Araguaia collisional orogeny (540-520 Ma), between an Amazonia craton group and the West Africa, Congo-Sao Francisco, Parana and Rio de la Plata cratons (Trindade et al., 2006 and references therein); (ii) The Amazonia craton group included the Arequipa-Antofalla and Western Sierras Pampeanas basement blocks (Rapela et al., 2007), for which a common metamorphic and magmatic history has been established (Casquet et al., 2006; 2008); (iii) Further evidence shows that the large Neoproterozoic turbiditic sequence of the Eastern Sierras Pampeanas (Pampean belt), now bounded to the east by the Palaeoproterozoic Rio de la Plata craton, is a transcurrent terrane resulting from right-lateral movements along the SW Gondwana margin (Rapela et al., 2007). This dextral displacement was associated with the oblique collision of the Western Sierras Pampeanas during the Pampean– Araguaia orogeny, following closure of the intervening Clymene ocean (Fig. 2); (iv) South" @default.
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- W129336873 date "2008-01-01" @default.
- W129336873 modified "2023-10-02" @default.
- W129336873 title "Revisiting accretionary history and magma sources in the SouthernAndes: Time variation of “typical Andean granites”" @default.
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