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Extension and general evolution of the Río de la Plata Craton
(Elsevier, 2009)
The Río de la Plata Craton (RPC) comprises part of southern Brazil, Paraguay, Uruguay and the central-eastern sector of Argentina. To the north, the RPC is bounded by the southern Amazonian craton, whereas to the east it ...
Precambrian geotectonic units of the Rio de La Plata craton
(TAYLOR & FRANCIS INC, 2010)
The main Precambrian tectonic units of Uruguay include the Piedra Alta tectonostratigraphic terrane (PATT) and Nico Perez tectonostratigraphic terrane (NPTT), separated by the Sarandi del Yi high-strain zone. Both terranes ...
Evolución paleogeográfica del cratón del Río de la Plata en el Precámbrico y su relación con el Terreno Pampia en el Cámbrico
(2019-03-14)
La evolución paleogeográfica del Cratón del Río de la Plata durante el Precámbrico presenta grandes interrogantes referidos a su participación en los supercontinentes proterozoicos Columbia y Rodinia y sobre su rol en la ...
Comment on: “Chemostratigraphic constraints on early Ediacaran carbonate ramp dynamics, Río de la Plata craton, Uruguay” by Aubet et al. Gondwana Research, Volume 22, Issues 3-4, November 2012, Pages 1073-1090
(Elsevier Science, 2013-04)
The Arroyo del Soldado Group of Uruguay is a key unit for unraveling several, still unsolved cardinal problems in Neoproterozoic research. Thus, we welcome in principle publications contributing to our knowledge of this ...
Formación Piedras de Afilar
(2014)
Formación Piedras de Afilar
(2014)
Electrical structure of the lithosphere from Rio de la Plata craton to Paraná basin: amalgamation of cratonic and refertilized lithospheres in SW Gondwanaland
(American Geophysical Union, 2019)
We conducted a magnetotelluric (MT) study from Paleoproterozoic Rio de la Plata Craton, in Uruguay, toward Paleozoic-Mesozoic Paraná Basin, in Brazil. The 850-km-long MT transect comprises 35 evenly spaced broadband ...
Neoproterozoic geodynamic evolution of SW-Gondwana: a southern African perspective
(SPRINGER, 2011)
Our current understanding of the tectonic history of the principal Pan-African orogenic belts in southwestern Africa, reaching from the West Congo Belt in the north to the Lufilian/Zambezi, Kaoko, Damara, Gariep and finally ...