Structural evolution of the Sarandí del Yí Shear Zone, Uruguay: kinematics, deformation conditions and tectonic significance

Author:

Oriolo S.,Oyhantçabal P.,Heidelbach F.,Wemmer K.,Siegesmund S.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences

Reference100 articles.

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2. Bak J, Kortsgård J, Sørensen K (1975) A major shear zone within the Nagssugtoqidian of west Greenland. Tectonophys 27:191–209

3. Basei MAS, Siga Jr O, Masquelin H, Harara OM, Reis Neto JM, Preciozzi F (2000) The Dom Feliciano Belt (Brazil–Uruguay) and its Foreland (Río de la Plata Craton): framework, tectonic evolution and correlations with similar terranes of southwestern Africa. In: Cordani U, Milani E, Thomaz Filho A, Campos D (eds) Tectonic evolution of South America. 31° International Geological Congress, Rio de Janeiro, pp 311–334

4. Basei MAS, Frimmel HE, Nutman AP, Preciozzi F, Jacob J (2005) A connection between the Neoproterozoic Dom Feliciano (Brazil/Uruguay) and Gariep (Namibia/South Africa) orogenic belts–evidence from a reconnaissance provenance study. Precambrian Res 139:195–221

5. Basei MAS, Frimmel HE, Nutman AP, Preciozzi F (2008) West Gondwana amalgamation based on detrital zircon ages from Neoproterozoic Ribeira and Dom Feliciano belts of South America and comparison with coeval sequences from SW Africa. In: Pankhurst RJ, Trouw RAJ, Brito Neves BB, de Wit MJ (eds) West Gondwana: Pre–Cenozoic correlations across the South Atlantic region. Geological Society of London Special Publications, London, 294, pp 239–256

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