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Argentina Granite Colours Click on image to view & hover over image for material name.
We describe an unusual example of rhythmically layered peraluminous granitic pegmatite locally developed in the intragranitic Potrerillos NYF pegmatites derived from the A-type host granites of the Las Chacras–Potrerillos batholith, Sierra de San Luis, Argentina.
The central-eastern part of the Sierra de Velasco (Sierras Pampeanas, NW Argentina) is formed by the large Huaco (40 × 30 km) and Sanagasta (25 × 15 km) granite massifs and the small La Chinchilla stock (2 × 2 km). The larger granites intrude into
The central-eastern part of the Sierra de Velasco (Sierras Pampeanas, NW Argentina) is formed by the large Huaco (40 × 30 km) and Sanagasta (25 × 15 km) granite massifs and the small La Chinchilla stock (2 × 2 km). The larger granites intrude into Ordovician metagranitoids and crosscut Devonian (?) mylonitic shear zones, whereas the small stock sharply intrudes into the Huaco granite.
2010. 8. 26. The granites were emplaced during three main orogenic events: (a) Pampean (mid-Cambrian), (b) Famatinian (Cambro-Ordovician), and (c) Achalian (Devonian-Carboniferous). This collaborative project, with Pablo Alasino and Juan
The Huaco and Sanagasta granites have a mainly crustal source, but with some participation of a more primitive, possibly mantle-derived, component. The main crustal component can be attributed to...
The Achala batholith is a post-orogenic intrusion of probable Silurian age exposed in the Sierra de Cordoba in the eastern Sierras Pampeanas of central Argentina (31°6′S to 32°2′S; 64°29′W to 65°7′W). The batholith was emplaced into late Precambrian amphibolite- and granulite-facies metamorphic rocks.
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In the case of the Argentina granites there is evidence of a significant crustal component. The Archean rift- related Kola granitoids overlap with the OIB field, but largely fall in the area dominated by crustal compositions. Note that in the case of both the Kola and Argentina granitoids there is also a possible IAB-like end-member.