Río de la Plata Craton
The Río de la Plata Craton (RPC) is a medium-sized continental block found in Uruguay, eastern Argentina and southern Brazil. During its complex and protracted history it interacted with a series other blocks and is therefore considered important for the understanding of the amalgamation of West Gondwana. Two orogenic cycles have been identified in the RPC: a 2000 Ma-old western domain representing the old craton and a 700–500 Ma-old eastern domain assigned to the Brasiliano Cycle.[1] It is one of the five cratons (ancient nuclei) of the South American continent. The other four cratons are: Amazonia, São Francisco, Río Apa and Arequipa–Antofalla.
Geology
Three shear zones divides the Precambrian basement of Uruguay and southern Brazil into four terranes.
Along the Uruguayan east coast (reaching into Brazil) is the Cuchilla Dionisio Terrane, an allochthonous African block juxtaposed to the RPC along the Sierra Ballena Shear Zone (SBSZ).[1]
West of Cuchilla Dionisio, the Nico Pérez Terrane is delimited by two longitudinal shear zones: the SBSZ and the Late Mesoporterozoic Sarandí del Yí Shear Zone (SYSZ). In the Nico Pérez Terrane, Neoproterzoic sedimentary successions crop out, probably deposited on an Atlantic-style continental shelf.[1]
East of the SYSZ, the latitudinal Colonia Shear Zone (CSZ) separates the Palaeoproterozoic (2000±100 Ma) Piedra Alta Terrane to the north from the Tandilia Terrane to the south. The 1790±5 Ma-old Late Palaeoproterozoic Piedra Alta mafic dike swarm was affected by the 8 km (5.0 mi)-wide Mesoproterozoic SYSZ and its eastern end bends along the dextral megashear zone.[1]
Tectonic evolution
2.0 Ga Río de la Plata formed part of the Atlantica supercontinent, the first "West Gondwana".[2] Today it crops out in southern Uruguay and parts of Argentina. Crystalline rocks of the Río de la Plata Craton are dated between 2200 and 1700 million years ago, such as rocks in Uruguay which are dated at 1790 ±5 Ma.[3] Dikes trending ENE in the same area are dated by argon-argon dating at 1727 ±10 Ma.[4] The craton has a size of about 20,000 square kilometres.
West Gondwana was assembled along the Transbrasiliano lineament in the Mid-Cambrian as, on one side, Amazonia, Río Apa, and some minor blocks collided with, on the other side, São Francisco/Congo, Río de la Plata, and some minor blocks. South of this lineament, along the western margin of the Río de la Plata Craton, the 535-520 Ma-old Pampean orogeny is partly made of an exotic terrane that was accreted to Gondwana's proto-Pacific margin (i.e. before the Andes had formed.)[5]
The Adamastor Ocean, a "proto-Atlantic" ocean that opened with the break-up of the Rodinia supercontinent 780-750 Ma, separated the Río de la Plata Craton from the Congo Craton. The inversion of the Adamastor Ocean began 640 Ma with the development of a large back-arc basin along the western margin of the Kalahari Craton and the ocean closed when Río de la Plata collided with Kalahari about 545 Ma along the sinistral Sierra Ballena Shear Zone.[6] The São Francisco and Río de la Plata plates amalgamated 630–620 Ma, closing the Adamastor Ocean on the South American side and forming the Mantiqueira Mountains around 600 Ma.[7]
References
Notes
- ↑ 1.0 1.1 1.2 1.3 Gaucher et al. 2008, Introduction, pp. 151–152
- ↑ Geraldes, Tavares & Dos Santos 2015, pp. 1064–1065
- ↑ Halls et al. 2001
- ↑ Teixeira et al. 1999
- ↑ Rapela et al. 2007, Introduction, pp. 50–52
- ↑ Rapela et al. 2007, 7.6 Tectonic Model, p. 76
- ↑ Brito Neves, Campos Neto & Fuck 1999, Mantiqueira branched systems of orogens, pp. 161–162
Sources
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